Publications - Tomas Capaldi

%7B%22status%22%3A%22success%22%2C%22updateneeded%22%3Afalse%2C%22instance%22%3Afalse%2C%22meta%22%3A%7B%22request_last%22%3A0%2C%22request_next%22%3A0%2C%22used_cache%22%3Atrue%7D%2C%22data%22%3A%5B%7B%22key%22%3A%225339SD9L%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Odlum%20et%20al.%22%2C%22parsedDate%22%3A%222024-02-21%22%2C%22numChildren%22%3A0%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EOdlum%2C%20M.%20L.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Thomson%2C%20K.%20D.%2C%20%26amp%3B%20Stockli%2C%20D.%20F.%20%282024%29.%20Tracking%20cycles%20of%20Phanerozoic%20opening%20and%20closing%20of%20ocean%20basins%20using%20detrital%20rutile%20and%20zircon%20geochronology%20and%20geochemistry.%20%3Ci%3EGeology%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FG51826.1%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FG51826.1%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Tracking%20cycles%20of%20Phanerozoic%20opening%20and%20closing%20of%20ocean%20basins%20using%20detrital%20rutile%20and%20zircon%20geochronology%20and%20geochemistry%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Margaret%20L.%22%2C%22lastName%22%3A%22Odlum%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Tomas%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Kelly%20D.%22%2C%22lastName%22%3A%22Thomson%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Daniel%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%5D%2C%22abstractNote%22%3A%22Sedimentary%20basins%20provide%20a%20deep%20time%20archive%20of%20tectonic%20and%20Earth-surface%20processes%20that%20can%20be%20leveraged%20by%20detrital%20mineral%20U-Pb%20dating%20and%20geochemistry%20to%20track%20paleogeography%2C%20magmatism%2C%20and%20crustal%20evolution.%20Zircon%20preserves%20the%20long-term%20%28billions%20of%20years%29%20record%20of%20supercontinent%20cycles%3B%20however%2C%20it%20is%20biased%20toward%20preserving%20felsic%20crustal%20records.%20Detrital%20rutile%20complements%20the%20detrital%20zircon%20record%20by%20providing%20constraints%20on%20the%20time%20and%20temperature%20of%20rifting%20and%20mafic%20magmatism%2C%20metamorphism%2C%20exhumation%20of%20the%20middle%20and%20lower%20crust%2C%20subduction%2C%20and%20amagmatic%20orogenesis.%20We%20use%20detrital%20zircon%20U-Pb%20and%20detrital%20rutile%20U-Pb%20geochronology%20and%20trace%20element%20analysis%20of%20Permian%20to%20Eocene%20siliciclastic%20rocks%20in%20the%20southern%20Pyrenees%20to%20capture%20supercontinent%20cycles%20of%20ocean%20basins%20opening%20and%20closing.%20Detrital%20rutile%20age%20spectra%20show%20peaks%20at%20ca.%20100%20Ma%20associated%20with%20rifting%20and%20hyperextension%20in%20the%20Pyrenean%20realm%2C%20200%20Ma%20associated%20with%20the%20Central%20Atlantic%20Magmatic%20Province%2C%20and%20330%20Ma%2C%20375%20Ma%2C%20and%20400%20Ma%20associated%20with%20subduction%20and%20Rheic%20Ocean%20crust%20formation.%20Zr-in-rutile%20thermometry%20and%20rutile%20Cr-Nb%20systematics%20provide%20further%20insight%20into%20metamorphic%20facies%20%28peak%20metamorphic%20temperatures%29%20and%20source%20rock%20lithology%20%28mafic%20versus%20felsic%20affinity%29.%20Detrital%20zircon%20age%20spectra%20have%20peaks%20at%20ca.%20300%20Ma%2C%20450%20Ma%2C%20and%20600%20Ma%20associated%20with%20major%20orogenic%20events%20and%20felsic%20magmatism%2C%20and%20Th%5C%2FU%20ratios%20provide%20information%20on%20relative%20zircon%20formation%20temperatures.%20Comparison%20of%20these%20independent%20records%20shows%20that%20detrital%20rutile%20reflects%20rifting%2C%20magma-poor%20orogenesis%2C%20and%20oceanic%20lithospheric%20processes%2C%20while%20detrital%20zircon%20detects%20continental%20lithospheric%20processes.%20Integrated%20detrital%20zircon%20and%20rutile%20data%20sets%20archive%20past%20geological%20events%20across%20multiple%20Wilson%20cycles.%22%2C%22date%22%3A%222024-02-21%22%2C%22language%22%3A%22en%22%2C%22DOI%22%3A%2210.1130%5C%2FG51826.1%22%2C%22ISSN%22%3A%220091-7613%2C%201943-2682%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fpubs.geoscienceworld.org%5C%2Fgeology%5C%2Farticle%5C%2Fdoi%5C%2F10.1130%5C%2FG51826.1%5C%2F635318%5C%2FTracking-cycles-of-Phanerozoic-opening-and-closing%22%2C%22collections%22%3A%5B%22BGC9F53I%22%2C%228MGFHE4Z%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A15%3A37Z%22%7D%7D%2C%7B%22key%22%3A%22CDCZZCDB%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Starck%20et%20al.%22%2C%22parsedDate%22%3A%222024%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EStarck%2C%20D.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Fuentes%2C%20F.%2C%20%26amp%3B%20Horton%2C%20B.%20K.%20%282024%29.%20Tectonic%20and%20climatic%20significance%20of%20Oligocene-Miocene%20eolian%20sandstones%20in%20the%20Andean%20foreland%20basin%20of%20Argentina.%20%3Ci%3EJournal%20of%20South%20American%20Earth%20Sciences%3C%5C%2Fi%3E%2C%20%3Ci%3E134%3C%5C%2Fi%3E%2C%2020.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.jsames.2023.104758%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.jsames.2023.104758%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Tectonic%20and%20climatic%20significance%20of%20Oligocene-Miocene%20eolian%20sandstones%20in%20the%20Andean%20foreland%20basin%20of%20Argentina%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%22%2C%22lastName%22%3A%22Starck%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22F.%22%2C%22lastName%22%3A%22Fuentes%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%5D%2C%22abstractNote%22%3A%22Late%20Oligocene-early%20Miocene%20aridification%20in%20the%20retroarc%20foreland%20basin%20adjacent%20to%20the%20southern%20central%20Andes%20was%20recorded%20by%20widespread%20eolian%20conditions%20that%20coincided%20with%20accelerated%20subsidence%20driven%20by%20the%20main%20phase%20of%20Andean%20tectonic%20loading.%20An%20extensive%20eolian%20dune%20system%2C%20which%20is%20rare%20in%20most%20foreland%20basins%2C%20indicates%20specific%20conditions%20in%20terms%20of%20climate%20%28aridity%29%2C%20atmospheric%20circulation%2C%20orography%2C%20sediment%20sources%2C%20dispersal%20patterns%2C%20and%20accommodation%20space.%20Detrital%20zircon%20U-Pb%20geochronological%20results%20for%20eolian%20sandstones%20spanning%2020%20foreland%20localities%20in%20northwestern%20to%20west-central%20Argentina%2C%20from%2022S%20to%2036S%2C%20reveal%20relatively%20localized%20Andean%20sources%20rather%20than%20regional%20cratonic%20provenance.%20Clastic%20detritus%20was%20largely%20derived%20from%20Phanerozoic%20igneous%20and%20sedimentary%20rocks%20of%20the%20Andean%20magmatic%20arc%20and%20retroarc%20fold-thrust%20belt%20during%20initial%20shortening-induced%20uplift%20of%20hinterland%20regions%20such%20as%20the%20Western%20Cordillera%2C%20Principal%20Cordillera%2C%20and%20Frontal%20Cordillera.%20This%20provenance%20record%20provides%20the%20earliest%20evidence%20for%20major%20westerly%20winds%2C%20transporting%20Andean%20detritus%20broadly%20eastward%20to%20the%20foreland%20basin%20%28with%20common%20axial%20northward%20deflections%29%20during%20a%20climate%20shift%20marked%20by%20the%20latest%20Oligocene-earliest%20Miocene%20inception%20of%20arid%20conditions.%20In%20addition%20to%20the%20climatic%20implications%2C%20independent%20stratigraphic%20data%20provide%20the%20basis%20for%20a%20compilation%20of%20sediment%20accumulation%20histories%20showing%20that%20eolian%20deposition%20was%20synchronous%20with%20accelerated%20subsidence%20attributable%20to%20enhanced%20Andean%20shortening.%20We%20propose%20that%20accelerated%20Andean%20uplift%20in%20the%20latest%20Oligocene-early%20Miocene%20generated%20rain-shadow%20conditions%20contemporaneous%20with%20increased%20sediment%20accommodation%20in%20the%20foreland%20basin%2C%20underscoring%20the%20important%20influence%20of%20tectonic%20processes%20on%20regional%20climate.%22%2C%22date%22%3A%222024%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1016%5C%2Fj.jsames.2023.104758%22%2C%22ISSN%22%3A%220895-9811%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22BWBMHIUE%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Plonka%20et%20al.%22%2C%22parsedDate%22%3A%222023-09%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EPlonka%2C%20Z.%20C.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Odlum%2C%20M.%20L.%2C%20Mackaman-Lofland%2C%20C.%2C%20Ortiz%2C%20G.%2C%20%26amp%3B%20Alvarado%2C%20P.%20%282023%29.%20Along-strike%20tectonic%20evolution%20of%20the%20Neogene%20Bermejo%20foreland%20basin%20and%20Eastern%20Precordillera%20thrust%20front%2C%20Argentina%20%2830-32%26%23xB0%3BS%29.%20%3Ci%3EJournal%20of%20South%20American%20Earth%20Sciences%3C%5C%2Fi%3E%2C%20%3Ci%3E129%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.jsames.2023.104521%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.jsames.2023.104521%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Along-strike%20tectonic%20evolution%20of%20the%20Neogene%20Bermejo%20foreland%20basin%20and%20Eastern%20Precordillera%20thrust%20front%2C%20Argentina%20%2830-32%5Cu00b0S%29%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Z.%20C.%22%2C%22lastName%22%3A%22Plonka%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20L.%22%2C%22lastName%22%3A%22Odlum%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22G.%22%2C%22lastName%22%3A%22Ortiz%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22P.%22%2C%22lastName%22%3A%22Alvarado%22%7D%5D%2C%22abstractNote%22%3A%22The%20Bermejo%20retroarc%20foreland%20basin%20system%20formed%20in%20flexural%20response%20to%20Cenozoic%20crustal%20thickening%20in%20the%20Andean%20orogenic%20system%2C%20specifically%2C%20the%20eastward%20propagation%20of%20the%20Precordillera%20fold-thrust%20belt%20and%20the%20basement-involved%20uplift%20of%20the%20Sierras%20Pampeanas.%20Previous%20work%20in%20the%20region%20has%20mainly%20focused%20on%20the%20mechanisms%20and%20expression%20of%20flat%20slab%20subduction%20and%20the%20structural%20geometry%20of%20the%20basement-involved%20Sierras%20Pampeanas%20and%20east-directed%20Precordillera%20fold-thrust%20belt%20at%20depth%2C%20advancing%20our%20understanding%20of%20the%20Bermejo%20basin%20history%20north%20of%2031%20%26%20DEG%3BS.%20However%2C%20the%20along%20strike%20evolution%20of%20the%20basin%20system%20to%20the%20south%20remains%20unresolved%20and%20contrasting%20tectonic%20models%20have%20proposed%20the%20Bermejo%20basin%20evolved%20synchronously%20versus%20asynchronously%20through%20time.%20Our%20study%20seeks%20to%20constrain%20the%20along-strike%20Neogene%20tectonics%20of%20the%20Bermejo%20basin%20via%20well-exposed%20Miocene%20fluvial%20stratigraphic%20intervals%20along%20the%20Eastern%20Precordillera%2C%20integrated%20with%20detrital%20zircon%20U-Pb%20geochronology%20provenance%20and%20detrital%20apatite%20%28U-Th%29%5C%2FHe%20thermochronology%20datasets.%20New%20data%20from%20two%20Neogene%20stratigraphic%20sections%20in%20the%20southern%20Bermejo%20basin%20constrain%20deposition%20between%2013%20and%206%20Ma.%20Dominant%20fluvial-lacustrine%20mudstones%2C%20siltstones%2C%20and%20sandstones%20transition%20into%20fluvial-megafan%20deposits%20capped%20by%20alluvial%20fan%20conglomerate%20facies%2C%20tracking%20the%20eastward%20migration%20of%20Precordillera%20deformation.%20The%20cessation%20of%20sedimentation%2C%20and%20thermal%20history%20models%20of%20apatite%20%28U-Th-Sm%29%5C%2FHe%20thermochronology%20ages%2C%20indicates%20basin%20incorporation%20into%20the%20orogenic%20wedge%20by%206%20Ma.%20When%20we%20compare%20our%20southern%20datasets%20with%20previous%20constraints%20from%20the%20northern%20Bermejo%20basin%2C%20we%20observe%2C%20from%20north%20to%20south%3A%20%281%29%20a%20time-transgressive%20trend%20in%20basin%20initiation%2C%20%282%29%20a%20-3%20km%20decrease%20in%20stratigraphic%20thicknesses%2C%20and%20%283%29%20older%20exhumation%20along%20the%20thrust%20front.%20These%20trends%20highlight%20the%20asynchronous%20nature%20of%20the%20Bermejo%20foreland%20basin%20system%20and%20alongstrike%20variability%20of%20Precordillera%20thrust-front%20evolution.%22%2C%22date%22%3A%22Sep%202023%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1016%5C%2Fj.jsames.2023.104521%22%2C%22ISSN%22%3A%220895-9811%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%2C%228MGFHE4Z%22%5D%2C%22dateModified%22%3A%222024-03-14T18%3A53%3A25Z%22%7D%7D%2C%7B%22key%22%3A%22JLDDRUJZ%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Akciz%20et%20al.%22%2C%22parsedDate%22%3A%222023-04%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EAkciz%2C%20S.%20O.%2C%20Ludwig%2C%20L.%20G.%2C%20Arrowsmith%2C%20R.%20J.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20%26amp%3B%20Rhodes%2C%20E.%20J.%20%282023%29.%20Channel%20Incision%20Ages%20to%20the%20Rescue%3A%20An%20Improved%20Age%20for%20the%20Penultimate%20Earthquake%20That%20Ruptured%20the%20Carrizo%20Section%20of%20the%20South-%20Central%20San%20Andreas%20Fault.%20%3Ci%3EBulletin%20of%20the%20Seismological%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E113%3C%5C%2Fi%3E%282%29%2C%20877%26%23x2013%3B887.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1785%5C%2F0120220189%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1785%5C%2F0120220189%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Channel%20Incision%20Ages%20to%20the%20Rescue%3A%20An%20Improved%20Age%20for%20the%20Penultimate%20Earthquake%20That%20Ruptured%20the%20Carrizo%20Section%20of%20the%20South-%20Central%20San%20Andreas%20Fault%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22S.%20O.%22%2C%22lastName%22%3A%22Akciz%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22L.%20G.%22%2C%22lastName%22%3A%22Ludwig%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22R.%20J.%22%2C%22lastName%22%3A%22Arrowsmith%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22E.%20J.%22%2C%22lastName%22%3A%22Rhodes%22%7D%5D%2C%22abstractNote%22%3A%22A%20primary%20step%20toward%20assessing%20the%20time%20and%20size%20of%20future%20earthquakes%20is%20identifying%20earth-quake%20recurrence%20patterns%20in%20the%20seismic%20record.%20The%20San%20Andreas%20fault%20%28SAF%29%20is%20one%20of%20the%20most%20studied%20active%20faults%20in%20the%20world.%20However%2C%20there%20is%20no%20unequivocal%20interpretation%20of%20paleoseismic%20data%20to%20determine%20the%20timing%20and%20rupture%20extent%20of%20the%20earthquakes%20that%20occurred%20prior%20to%20the%20historical%201857%20and%201906%20ruptures.%20The%20penultimate%20earthquake%20is%20the%20least%20well-dated%20earthquake%20along%20the%20Cholame%2C%20Carrizo%2C%20and%20Big%20Bend%20sections%20of%20the%20SAF.%20The%20main%20reason%20for%20this%20poor%20determination%20is%20because%20the%20past%20few%20hundred%20years%20have%20seen%20large%20natural%20fluctuations%20in%20atmospheric%2014C%20concentration.%20These%20fluctuations%20mean%20that%20a%20single%20radiocarbon%20date%20may%20yield%20a%20calibrated%20age%20consisting%20of%20several%20possible%20age%20ranges.%20At%20sites%20along%20frequently%20rupturing%20faults%20with%20historical%20ruptures%2C%20such%20as%20the%20SAF%20and%20the%20North%20Anatolian%20fault%20in%20Turkey%2C%20determining%20the%20incision%20age%20of%20channels%20displaced%20only%20by%20the%20most%20recent%20earthquake%20can%20place%20a%20tighter%20minimum%20limit%20on%20the%20possible%20age%20range%20of%20the%20penultimate%20earthquake.%20In%20our%20study%2C%20we%20dated%20five%20sandy%20fill%20units%20with%20the%20post%20-infra-red%20infrared-stimulated%20luminescence%20method%20on%20single%20feldspar%20grains%20of%20channel%20Sieh%2031%20in%20the%20Carrizo%20Plain.%20The%20data%20indicate%20the%20channel%20Sieh%2031%2C%20offset%20-6%20m%20during%20the%201857%20earth-quake%2C%20incised%20before-1740%20%2B%5C%2F-%2030%20C.E.%20%281%20sigma%29.%20This%20new%20result%20trims%20the%20age%20constraint%20of%20the%20penultimate%20earthquake%20that%20ruptured%20the%20Carrizo%20section%20of%20the%20SAF%20determined%20at%20the%20nearby%20Bidart%20Fan%20site%20from%201640-1857%20to%201631-1745%20C.E.%2C%20tightening%20the%20age%20constraint%20by%20nearly%2080%20yr.%20The%20revised%20mean%20recurrence%20interval%20for%20surface%20rupturing%20earthquakes%20along%20the%20Carrizo%20section%20of%20the%20south-central%20SAF%20is%20117%20yr%20%2895%25%20confidence%20interval%2062-255%20yr%29.%20This%20approach%20can%20improve%20paleoearthquake%20age%20and%20slip-per-earthquake%20constraints.%22%2C%22date%22%3A%22Apr%202023%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1785%5C%2F0120220189%22%2C%22ISSN%22%3A%220037-1106%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22MZ6QWRDK%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Horton%20et%20al.%22%2C%22parsedDate%22%3A%222022-11%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EHorton%2C%20B.%20K.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Mackaman-Lofland%2C%20C.%2C%20Perez%2C%20N.%20D.%2C%20Bush%2C%20M.%20A.%2C%20Fuentes%2C%20F.%2C%20%26amp%3B%20Constenius%2C%20K.%20N.%20%282022%29.%20Broken%20foreland%20basins%20and%20the%20influence%20of%20subduction%20dynamics%2C%20tectonic%20inheritance%2C%20and%20mechanical%20triggers.%20%3Ci%3EEarth-Science%20Reviews%3C%5C%2Fi%3E%2C%20%3Ci%3E234%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20104193%2010.1016%5C%2Fj.earscirev.2022.104193%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20104193%2010.1016%5C%2Fj.earscirev.2022.104193%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Broken%20foreland%20basins%20and%20the%20influence%20of%20subduction%20dynamics%2C%20tectonic%20inheritance%2C%20and%20mechanical%20triggers%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%20D.%22%2C%22lastName%22%3A%22Perez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20A.%22%2C%22lastName%22%3A%22Bush%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22F.%22%2C%22lastName%22%3A%22Fuentes%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20N.%22%2C%22lastName%22%3A%22Constenius%22%7D%5D%2C%22abstractNote%22%3A%22Broken%20foreland%20basins%20are%20caused%20by%20crustal-scale%20contractional%20basement%20structures%20that%20compartmentalize%20%28or%20break%29%20a%20contiguous%20retroarc%20or%20collisional%20foreland%20basin%20into%20smaller%20disconnected%20basins.%20Broken%20foreland%20basins%20differ%20from%20their%20unbroken%20counterparts%20in%20their%20deformational%2C%20depositional%2C%20and%20geodynamic%20framework.%20Whereas%20contiguous%20%28unbroken%29%20foreland%20basins%20are%20generated%20mainly%20by%20regional%20flexural%20loading%20due%20to%20shortening%20of%20supracrustal%20cover%20strata%20and%20uppermost%20basement%20in%20organized%20ramp-flat%20thrust%20systems%2C%20broken%20foreland%20basins%20are%20governed%20principally%20by%20isolated%20topographic%20loads%20and%20structural%20tilting%20associated%20with%20widely%20spaced%20crustal-scale%20reverse%20faults%20that%20accommodate%20intraplate%20basement%20shortening.%20These%20structural%20contrasts%20foster%20either%20de%20acute%20accent%20collement-style%20fold-thrust%20belts%20%28orogenic%20wedges%29%20with%20large%20integrated%20erosional%20drainage%20systems%20%28watersheds%29%20spanning%20diverse%20sediment%20source%20regions%20%28including%20thin-skinned%20fold-thrust%20belts%2C%20elevated%20hinterland%20zones%2C%20accreted%20terranes%2C%20and%20magmatic%20arcs%29%20or%20independent%20foreland%20block%20uplifts%20with%20local%20drainage%20systems%20dominated%20by%20basement%20sources.%20Although%20the%20genesis%20of%20broken%20foreland%20basins%20has%20been%20uniquely%20attributed%20to%20flat%20slab%20subduction%2C%20these%20basins%20are%20also%20sensitive%20to%20inherited%20structural%2C%20strati%20-graphic%2C%20thermal%2C%20and%20rheological%20configurations%2C%20as%20well%20as%20synorogenic%20mass%20redistribution%20in%20relationship%20to%20climate%2C%20erosion%2C%20sediment%20transport%20efficiency%2C%20and%20sediment%20accumulation.Despite%20the%20many%20modern%20and%20ancient%20examples%2C%20questions%20persist%20over%20the%20underlying%20geodynamic%20processes%20that%20promote%20development%20of%20a%20broken%20or%20compartmentalized%20foreland%20basin%20instead%20of%20a%20single%20regionally%20unified%20flexural%20foreland%20basin.%20Additional%20uncertainties%20and%20misconceptions%20surround%20the%20criteria%20used%20to%20define%20broken%20foreland%20basins%20and%20their%20linkages%20to%20subduction%20dynamics%20%28chiefly%20slab%20geometry%29%2C%20strain%20magnitude%2C%20and%20structural%20reactivation.%20Here%20we%20review%20the%20tectonic%20framework%20of%20broken%20foreland%20basins-with%20emphasis%20on%20South%20and%20North%20America%20%28Pampean%20and%20Laramide%20provinces%29-and%20propose%20that%20their%20genesis%20can%20be%20ascribed%20to%20a%20combination%20of%3A%20%28i%29%20underlying%20conditions%20in%20the%20form%20of%20tectonic%20inheritance%2C%20including%20precursor%20structural%2C%20stratigraphic%2C%20thermal%2C%20and%20rheological%20heterogeneities%20and%20anisotropies%3B%20and%20%28ii%29%20mechanical%20triggers%2C%20such%20as%20increased%20stress%2C%20enhanced%20horizontal%20stress%20transmission%2C%20and%5C%2For%20selective%20crustal%20strengthening%20or%20weakening.%22%2C%22date%22%3A%22Nov%202022%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20104193%2010.1016%5C%2Fj.earscirev.2022.104193%22%2C%22ISSN%22%3A%220012-8252%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%228K8XT4XZ%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222022-10%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Odlum%2C%20M.%20L.%2C%20Curry%2C%20M.%20E.%2C%20%26amp%3B%20Stockli%2C%20D.%20F.%20%282022%29.%20Variable%20thermal%20histories%20across%20the%20Pyrenees%20orogen%20recorded%20in%20modern%20river%20sand%20detrital%20geo-%5C%2Fthermochronology%20and%20PECUBE%20thermokinematic%20modelling.%20%3Ci%3EBasin%20Research%3C%5C%2Fi%3E%2C%20%3Ci%3E34%3C%5C%2Fi%3E%285%29%2C%201781%26%23x2013%3B1806.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fbre.12685%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fbre.12685%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Variable%20thermal%20histories%20across%20the%20Pyrenees%20orogen%20recorded%20in%20modern%20river%20sand%20detrital%20geo-%5C%2Fthermochronology%20and%20PECUBE%20thermokinematic%20modelling%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20L.%22%2C%22lastName%22%3A%22Odlum%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20E.%22%2C%22lastName%22%3A%22Curry%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%5D%2C%22abstractNote%22%3A%22The%20Pyrenees%20Mountains%20are%20a%20classic%20example%20of%20a%20doubly-verging%20collisional%20orogenic%20system%20with%20flanking%20retro-%20and%20pro-foreland%20basin%20systems.%20Previous%20bedrock%20and%20detrital%20geo-%5C%2Fthermochronologic%20studies%20have%20observed%20magmatic%20and%20exhumation-related%20ages%20that%20reflect%20a%20complex%20thermo-tectonic%20evolution%20of%20the%20European%20and%20Iberian%20plate%20margins%20related%20to%20break-up%20and%20assembly%20of%20the%20Gondwana%2C%20Pangea%20and%20Pyrenean-Alpine%20orogenic%20cycles.%20This%20study%20integrates%20detrital%20zircon%2C%20rutile%20and%20apatite%20U-Pb%20dating%20and%2C%20detrital%20zircon%20and%20apatite%20%28U-Th%29%5C%2FHe%20dating%20from%20modern%20river%20sands%20from%20the%20northern%20and%20southern%20Pyrenees%2C%20with%20PECUBE%20thermokinematic%20modelling%20of%20bedrock%20cooling%20ages%20to%20simulate%20detrital%20age%20distributions%20in%20order%20to%20evaluate%3A%20%281%29%20regional%20patterns%20in%20long-term%20crustal%20processes%20associated%20with%20pre-Pyrenean%20crustal%20shortening%2C%20crustal%20thinning%20and%20magmatism%20along%20the%20Iberian%20and%20European%20plate%20margin%3B%20%282%29%20timing%20of%20regional%20cooling%20and%20inferred%20erosion%20related%20to%20Pyrenean%20orogenesis%3B%20and%20%283%29%20the%20exhumation%20processes%20associated%20with%20post-orogenic%20decay%20and%20erosion.%20Modern%20river%20multimineral%20detrital%20geo-%5C%2Fthermochronometry%20results%20are%20consistent%20with%20previous%20bedrock%20thermal%20history%20models%20and%20records%20punctuated%20Variscan%20and%20Pyrenean%20cooling%20events%20in%20the%20pro-wedge%20that%20contrasts%20with%20protracted%20Permian%20to%20Pliocene%20thermal%20history%20preserved%20in%20the%20retro-wedge%20of%20the%20orogen.%20Detrital%20age%20distributions%20from%20PECUBE%20modelling%20predict%20the%20Pyrenean%20age%20component%20in%20both%20detrital%20apatite%20and%20zircon%20%28U-Th%29%5C%2FHe%20age%20distributions%2C%20indicating%20the%20modelled%20exhumation%20patterns%20in%20the%20Axial%20Zone%20and%20Northern%20Pyrenean%20Zone%20can%20predict%20observed%20Pyrenean%20thermochronology%20ages.%20The%20presence%20of%20strong%20Pyrenean%20age%20peaks%20amongst%20the%20modern%20river%20sand%20and%20modelled%20detrital%20cooling%20age%20distributions%20suggests%20retro-wedge%20deformation%20and%20exhumation%20remained%20active%20during%20the%20main%20phase%20of%20pro-wedge%20activity%20and%20experienced%20significant%20orogenic%20decay.%20Isolated%20Miocene%20apatite%20He%20ages%20from%20the%20North%20Pyrenees%20modern%20river%20record%20post-orogenic%20cooling%2C%20due%20to%20tectonic%20mode%20switch%20to%20extension%20and%20%28or%29%20climate-driven%20enhanced%20exhumation.%22%2C%22date%22%3A%22Oct%202022%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1111%5C%2Fbre.12685%22%2C%22ISSN%22%3A%220950-091x%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%2C%228MGFHE4Z%22%5D%2C%22dateModified%22%3A%222024-03-14T18%3A29%3A30Z%22%7D%7D%2C%7B%22key%22%3A%22SJTI5TIP%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Horton%20et%20al.%22%2C%22parsedDate%22%3A%222022-09-01%22%2C%22numChildren%22%3A0%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EHorton%2C%20B.%20K.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20%26amp%3B%20Perez%2C%20N.%20D.%20%282022%29.%20The%20role%20of%20flat%20slab%20subduction%2C%20ridge%20subduction%2C%20and%20tectonic%20inheritance%20in%20Andean%20deformation.%20%3Ci%3EGeology%3C%5C%2Fi%3E%2C%20%3Ci%3E50%3C%5C%2Fi%3E%289%29%2C%201007%26%23x2013%3B1012.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FG50094.1%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FG50094.1%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22The%20role%20of%20flat%20slab%20subduction%2C%20ridge%20subduction%2C%20and%20tectonic%20inheritance%20in%20Andean%20deformation%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Brian%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Tomas%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Nicholas%20D.%22%2C%22lastName%22%3A%22Perez%22%7D%5D%2C%22abstractNote%22%3A%22Abstract%5Cn%20%20%20%20%20%20%20%20%20%20%20%20Convergent%20plate%20boundaries%20show%20sharp%20variations%20in%20orogenic%20width%20and%20extent%20of%20intraplate%20deformation.%20Analysis%20of%20late%20Cenozoic%20contractile%20deformation%20along%20the%20Andean%20mountain%20front%20and%20adjacent%20foreland%20highlights%20the%20contrasting%20degrees%20of%20deformation%20advance%20toward%20the%20plate%20interior.%20The%20retroarc%20positions%20of%20the%20Andean%20topographic%20front%20%28marked%20by%20frontal%20thrust-belt%20structures%29%20and%20foreland%20deformation%20front%20%28defined%20by%20isolated%20basement%20block%20uplifts%29%20range%20from%20300%20to%20900%20km%20inboard%20of%20the%20trench%20axis.%20Over%20the%20~8000%20km%20arcuate%20length%20of%20the%20Andes%20%2810%5Cu00b0N%20to%2055%5Cu00b0S%29%2C%20four%20discrete%20maxima%20of%20inboard%20deformation%20advance%20are%20spatially%20co-located%20with%20the%20Peruvian%20%285%5Cu00b0S%5Cu201314%5Cu00b0S%29%20and%20Pampean%20%2827%5Cu00b0S%5Cu201333%5Cu00b0S%29%20zones%20of%20flat%20slab%20subduction%2C%20the%20subducted%20Chile%20Ridge%20%2845%5Cu00b0S%5Cu201348%5Cu00b0S%29%2C%20and%20the%20anomalously%20thick%20Paleozoic%20stratigraphic%20wedge%20of%20Bolivia%20%2817%5Cu00b0S%20%5Cu201323%5Cu00b0S%29.%20The%20spatial%20correspondence%20of%20retroarc%20shortening%20with%20specific%20geodynamic%20configurations%20demonstrates%20the%20mechanical%20role%20of%20flat%20slab%20subduction%2C%20slab%20window%20development%2C%20and%20combined%20structural%20and%20stratigraphic%20geometries%20in%20shaping%20the%20orogenic%20architecture%20of%20Cordilleran%20margins%2C%20largely%20through%20lithospheric%20strengthening%2C%20weakening%2C%20and%5C%2For%20tectonic%20inheritance.%22%2C%22date%22%3A%222022-09-01%22%2C%22language%22%3A%22en%22%2C%22DOI%22%3A%2210.1130%5C%2FG50094.1%22%2C%22ISSN%22%3A%220091-7613%2C%201943-2682%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fpubs.geoscienceworld.org%5C%2Fgeology%5C%2Farticle%5C%2F50%5C%2F9%5C%2F1007%5C%2F614055%5C%2FThe-role-of-flat-slab-subduction-ridge-subduction%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-05T16%3A48%3A43Z%22%7D%7D%2C%7B%22key%22%3A%22BIQAK7N9%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Garzanti%20et%20al.%22%2C%22parsedDate%22%3A%222022-08%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EGarzanti%2C%20E.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%2C%20Tripaldi%2C%20A.%2C%20Zarate%2C%20M.%2C%20Limonta%2C%20M.%2C%20%26amp%3B%20Vezzoli%2C%20G.%20%282022%29.%20Andean%20retroarc-basin%20dune%20fields%20and%20Pampean%20Sand%20Sea%20%28Argentina%29%3A%20Provenance%20and%20drainage%20changes%20driven%20by%20tectonics%20and%20climate.%20%3Ci%3EEarth-Science%20Reviews%3C%5C%2Fi%3E%2C%20%3Ci%3E231%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20104077%2010.1016%5C%2Fj.earscirev.2022.104077%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20104077%2010.1016%5C%2Fj.earscirev.2022.104077%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Andean%20retroarc-basin%20dune%20fields%20and%20Pampean%20Sand%20Sea%20%28Argentina%29%3A%20Provenance%20and%20drainage%20changes%20driven%20by%20tectonics%20and%20climate%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22E.%22%2C%22lastName%22%3A%22Garzanti%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22A.%22%2C%22lastName%22%3A%22Tripaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%22%2C%22lastName%22%3A%22Zarate%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%22%2C%22lastName%22%3A%22Limonta%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22G.%22%2C%22lastName%22%3A%22Vezzoli%22%7D%5D%2C%22abstractNote%22%3A%22We%20here%20review%20in%20terms%20of%20tectono-magmatic%20setting%20and%20Quaternary%20landscape%20dynamics%20what%20is%20known%20about%20the%20provenance%20of%20Argentine%20dune%20fields%20and%20their%20fluvial%20feeder%20systems%20draining%20the%20Andean%20Cordillera.%20The%20detrital%20signatures%20of%20these%20eolian%20sediments%20were%20previously%20investigated%20based%20on%20either%20framework%20petrography%20and%20heavy%20minerals%20or%20detrital-zircon%20geochronology%2C%20and%20their%20peculiar%20volcaniclastic%20nature%20was%20long%20recognized.%20Compositional%20variability%2C%20however%2C%20was%20only%20broadly%20evaluated%2C%20and%20quantitative%20provenance%20analysis%20based%20on%20a%20systematic%20multimethod%20approach%20across%20the%20entire%20region%20was%20not%20carried%20out%20so%20far.%20For%20this%20reason%2C%20here%20we%20integrate%20original%20and%20previously%20obtained%20petrographic%2C%20heavy-mineral%2C%20and%20detrital-zircon%20geochronology%20data%20to%20present%20the%20first%20comprehensive%20provenance%20study%20of%20dune%20fields%20stretching%20for%201000%20km%20across%20central%20Argentina%20from%20the%20Andean%20piedmont%20to%20the%20Atlantic%20Ocean.%20In%20dune%20fields%20along%20the%20Andean%20retroarc%20basin%2C%20sediment%20composition%20defines%20a%20steady%20northward%20decrease%20in%20volcanic%20detritus.%20This%20reflects%20active%20magmatism%20in%20the%20Southern%20Volcanic%20Zone%20and%20Payenia%20province%20%2838-34S%29%2C%20in%20contrast%20with%20the%20similar%20to%20600-km-long%20Pliocene-Quaternary%20magmatic%20gap%20in%20the%20Pampean%20flat-slab%20segment%20%2833-27S%29%2C%20where%20sediment%20is%20derived%20from%20deeper-seated%20tectono-stratigraphic%20levels%20of%20the%20continental%20arc%20and%20uplifted%20blocks%20of%20retroarc-basin%20basement.%20In%20distal%20Pampean%20lowlands%20extending%20across%20the%20bulge%20and%20backbulge%20depozones%2C%20instead%2C%20sand%20dunes%20display%20notably%20homogeneous%20compositional%20signatures%2C%20indicating%20that%20detritus%20was%20mostly%20generated%20north%20of%2034S%20and%20transported%20by%20a%20paleo-Desaguadero%20trunk%20river%20that%20formed%20during%20southward-progressing%20diachronous%20uplift%20of%20the%20Sierras%20Pampeanas%20since%20the%20late%20Miocene.%20In%20contrast%20with%20huge%20African%20and%20Arabian%20deserts%20that%20contain%20multiply%20recycled%20quartzose%20to%20pure%20quartzose%20sand%2C%20even%20very%20fragile%20volcanic%20clasts%2C%20plagioclase%20feldspar%2C%20and%20unstable%20ferromagnesian%20minerals%20are%20widespread%2C%20testifying%20to%20largely%20first-cycle%20volcanic%20provenance%20and%20only%20minor%20effects%20of%20mechanical%20breakdown%20and%20chemical%20weathering%20in%20the%20Pampean%20Sand%20Sea.%20During%20the%20Late%20Pleistocene%2C%20after%20a%20first%20southward%20shift%20of%20the%20Desaguadero%20trunk%20river%20possibly%20induced%20by%20increased%20water%20and%20sediment%20discharge%20at%20the%20end%20of%20the%20penultimate%20glacial%20maximum%2C%20tectonic%20uplift%20eventually%20outpaced%20stream%20power%20during%20the%20last%20glacial%20period.%20Paleo-rivers%20were%20thus%20forced%20to%20shift%20farther%20southwards%2C%20leading%20to%20the%20formation%20of%20an%20integrated%20paleo-Desaguadero%2BColorado%20drainage%20system.%20During%20the%20latest%20Pleistocene-early%20Holocene%2C%20such%20a%20large%20trunk%20river%20fostered%20the%20rapid%20progradation%20of%20a%20wide%20delta%20and%20littoral%20sand%20transport%20all%20along%20the%20shores%20of%20the%20Buenos%20Aires%20Province.%20Climate%20change%20and%20repeated%20waxing%20and%20waning%20of%20glaciers%20through%20the%20Quaternary%20have%20left%20a%20prominent%20mark%20on%20sediment%20distribution%2C%20dominated%20by%20fluvial%20processes%20during%20periods%20of%20high%20fluvial%20discharge%20but%20alternating%20with%20arid%20phases%20characterized%20by%20limited%20transport%20capacity%20and%20vegetation%20cover%2C%20extensive%20wind%20deflation%20of%20floodplains%2C%20and%20sand%20accumulation%20in%20the%20dune%20fields.%22%2C%22date%22%3A%22Aug%202022%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20104077%2010.1016%5C%2Fj.earscirev.2022.104077%22%2C%22ISSN%22%3A%220012-8252%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22MVVALA23%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222022-08%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Rittenour%2C%20T.%20M.%2C%20%26amp%3B%20Nelson%2C%20M.%20S.%20%282022%29.%20Downstream%20changes%20in%20quartz%20OSL%20sensitivity%20in%20modern%20river%20sand%20reflects%20sediment%20source%20variability%3A%20Case%20studies%20from%20Rocky%20Mountain%20and%20Andean%20rivers.%20%3Ci%3EQuaternary%20Geochronology%3C%5C%2Fi%3E%2C%20%3Ci%3E71%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20101317%2010.1016%5C%2Fj.quageo.2022.101317%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20101317%2010.1016%5C%2Fj.quageo.2022.101317%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Downstream%20changes%20in%20quartz%20OSL%20sensitivity%20in%20modern%20river%20sand%20reflects%20sediment%20source%20variability%3A%20Case%20studies%20from%20Rocky%20Mountain%20and%20Andean%20rivers%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20M.%22%2C%22lastName%22%3A%22Rittenour%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20S.%22%2C%22lastName%22%3A%22Nelson%22%7D%5D%2C%22abstractNote%22%3A%22OSL%20%28optically%20stimulated%20luminescence%29%20sensitivity%20of%20quartz%20has%20been%20shown%20to%20either%20%281%29%20record%20downstream%20sediment%20transport%20related%20to%20increased%20number%20and%20duration%20of%20light%20exposure%20cycles%20or%20%282%29%20be%20a%20function%20of%20source%20geology%2C%20presenting%20a%20potential%20tool%20to%20track%20sediment%20provenance.%20To%20test%20these%20competing%20models%20this%20study%20leverages%20a%20suite%20of%20modern%20river%20samples%20from%20an%20extensional%20basin%20system%20in%20the%20Rocky%20Mountains%20of%20western%20USA%20%28Bear%20River%29%20and%20a%20retroarc%20foreland%20basin%20system%20in%20the%20southern%20Central%20Andes%20of%20Argentina%20%28Rio%20San%20Juan%29%20to%20understand%20the%20relationships%20among%20quartz%20luminescence%20sensitivity%2C%20sediment%20transport%20distance%2C%20and%20catchment%20lithologies.%20We%20compare%20our%20results%20with%20petrographic%20analysis%20of%20the%20river%20sand%20composition%2C%20and%20characterization%20of%20the%20lithology%20and%20morphometrics%20of%20the%20river%20catchments.%20Samples%20taken%20along%20the%20Bear%20River%20and%20its%20major%20tributaries%20in%20the%20Rocky%20Mountains%20show%20a%20progressive%20downstream%20decrease%20in%20quartz%20OSL%20sensitivity%20that%20records%20variation%20in%20sediment%20provenance%20and%20steady%20contribution%20of%20lower%20OSL%20sensitivity%20quartz%20recycled%20from%20Palaeozoic%20passive%20margin%20stratigraphy.%20Andean%20river%20sand%20samples%20from%20the%20Rio%20San%20Juan%20network%20exhibit%20pervasive%20low%20sensitivity%20quartz%20derived%20from%20Andean%20arc%20volcanic%20rocks%20and%20recycled%20Neogene%20foreland%20basin%20strata.%20These%20modern%20river%20sand%20data%20do%20not%20show%20increased%20sensitivity%20with%20transport%20distance%20and%20instead%20indicates%20that%20in%20these%20landscapes%2C%20quartz%20OSL%20sensitivity%20is%20an%20intrinsic%20property%20of%20the%20source%20rock.%20Our%20study%20shows%20that%20river%20sands%20primarily%20composed%20of%20older%2C%20recycled%20low-strained%20quartz%20derived%20from%20quartzite%20lithologies%20exhibit%20the%20highest%20quartz%20sensitivity%20values.%20Moderate%20quartz%20OSL%20sensitivity%20values%20are%20observed%20in%20rivers%20with%20young%20igneous%20quartz%20derived%20directly%20from%20the%20volcanic%20and%20intrusive%20rocks.%20Conversely%2C%20micro%20crystalline%20quartz%20in%20chert%20lithic%20grains%20or%20polycrystalline%20quartz%20found%20in%20composite%20metamorphic%20lithic%20grains%20record%20the%20lowest%20quartz%20OSL%20sensitivity%20values.%20Determining%20the%20controlling%20factors%20of%20quartz%20sensitivity%20in%20river%20sand%20provides%20a%20current%20baseline%20for%20resolving%20paleogeographic%20and%20paleodrainage%20histories%20in%20the%20sedimentary%20record%20and%20provides%20further%20understanding%20of%20how%20sediments%20are%20eroded%2C%20transported%2C%20and%20deposited%20in%20fluvial%20systems%20with%20diverse%20tectonic%20settings%20and%20geologic%20source%20rocks.%22%2C%22date%22%3A%22Aug%202022%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20101317%2010.1016%5C%2Fj.quageo.2022.101317%22%2C%22ISSN%22%3A%221871-1014%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22NVJ87GQB%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Mackaman-Lofland%20et%20al.%22%2C%22parsedDate%22%3A%222022-08%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EMackaman-Lofland%2C%20C.%2C%20Horton%2C%20B.%20K.%2C%20Ketcham%2C%20R.%20A.%2C%20McQuarrie%2C%20N.%2C%20Fosdick%2C%20J.%20C.%2C%20Fuentes%2C%20F.%2C%20Constenius%2C%20K.%20N.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Stockli%2C%20D.%20F.%2C%20%26amp%3B%20Alvarado%2C%20P.%20%282022%29.%20Causes%20of%20Variable%20Shortening%20and%20Tectonic%20Subsidence%20During%20Changes%20in%20Subduction%3A%20Insights%20From%20Flexural%20Thermokinematic%20Modeling%20of%20the%20Neogene%20Southern%20Central%20Andes%20%2828-30%26%23xB0%3BS%29.%20%3Ci%3ETectonics%3C%5C%2Fi%3E%2C%20%3Ci%3E41%3C%5C%2Fi%3E%288%29.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2022TC007334%2010.1029%5C%2F2022TC007334%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2022TC007334%2010.1029%5C%2F2022TC007334%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Causes%20of%20Variable%20Shortening%20and%20Tectonic%20Subsidence%20During%20Changes%20in%20Subduction%3A%20Insights%20From%20Flexural%20Thermokinematic%20Modeling%20of%20the%20Neogene%20Southern%20Central%20Andes%20%2828-30%5Cu00b0S%29%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22R.%20A.%22%2C%22lastName%22%3A%22Ketcham%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%22%2C%22lastName%22%3A%22McQuarrie%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%20C.%22%2C%22lastName%22%3A%22Fosdick%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22F.%22%2C%22lastName%22%3A%22Fuentes%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20N.%22%2C%22lastName%22%3A%22Constenius%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22P.%22%2C%22lastName%22%3A%22Alvarado%22%7D%5D%2C%22abstractNote%22%3A%22The%20Andes%20of%20western%20Argentina%20record%20spatiotemporal%20variations%20in%20morphology%2C%20basin%20geometry%2C%20and%20structural%20style%20that%20correspond%20with%20changes%20in%20crustal%20inheritance%20and%20convergent%20margin%20dynamics.%20Above%20the%20modern%20Pampean%20flat-slab%20subduction%20segment%20%2827-33%20degrees%20S%29%2C%20retroarc%20shortening%20generated%20a%20fold-thrust%20belt%20and%20intraforeland%20basement%20uplifts%20that%20converge%20north%20of%20similar%20to%2029%20degrees%20S%2C%20providing%20opportunities%20to%20explore%20the%20effects%20of%20varied%20deformation%20and%20subduction%20regimes%20on%20synorogenic%20sedimentation.%20We%20integrate%20new%20detrital%20zircon%20U-Pb%20and%20apatite%20%28U-Th%29%5C%2FHe%20analyses%20with%20sequentially%20restored%2C%20flexurally%20balanced%20cross%20sections%20and%20thermokinematic%20models%20at%20similar%20to%2028.5-30%20degrees%20S%20to%20link%20deformation%20with%20resulting%20uplift%2C%20erosion%2C%20and%20basin%20accumulation%20histories.%20Tectonic%20subsidence%2C%20topographic%20evolution%2C%20and%20thermochronometric%20cooling%20records%20point%20to%20%28a%29%20shortening%20and%20distal%20foreland%20basin%20accumulation%20at%20similar%20to%2018-16%20Ma%2C%20%28b%29%20thrust%20belt%20migration%2C%20changes%20in%20sediment%20provenance%2C%20and%20enhanced%20flexural%20subsidence%20from%20similar%20to%2016%20to%209%20Ma%2C%20%28c%29%20intraforeland%20basement%20deformation%2C%20local%20flexure%2C%20and%20drainage%20reorganization%20at%20similar%20to%2012-7%20Ma%2C%20and%20%28d%29%20out-of-sequence%20shortening%20and%20exhumation%20of%20foreland%20basin%20fill%20by%20similar%20to%208-2%20Ma.%20Thrust%20belt%20kinematics%20and%20the%20reactivation%20of%20basement%20heterogeneities%20strongly%20controlled%20tectonic%20load%20configurations%20and%20subsidence%20patterns.%20Geo%5C%2Fthermochronological%20data%20and%20model%20results%20resolve%20increased%20shortening%20and%20combined%20thrust%20belt%20and%20intraforeland%20basement%20loading%20in%20response%20to%20ridge%20collision%20and%20Neogene%20shallowing%20of%20the%20subducted%20oceanic%20slab.%20Finally%2C%20this%20study%20demonstrates%20the%20utility%20of%20integrated%20flexural%20thermokinematic%20and%20erosion%20modeling%20for%20evaluating%20the%20geometries%2C%20rates%2C%20and%20potential%20drivers%20of%20retroarc%20deformation%20and%20foreland%20basin%20evolution%20during%20changes%20in%20subduction.%22%2C%22date%22%3A%22Aug%202022%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20e2022TC007334%2010.1029%5C%2F2022TC007334%22%2C%22ISSN%22%3A%220278-7407%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22I7VB8SC8%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Garzanti%20et%20al.%22%2C%22parsedDate%22%3A%222021-12%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EGarzanti%2C%20E.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%2C%20Vezzoli%2C%20G.%2C%20Limonta%2C%20M.%2C%20%26amp%3B%20Sosa%2C%20N.%20%282021%29.%20Transcontinental%20retroarc%20sediment%20routing%20controlled%20by%20subduction%20geometry%20and%20climate%20change%20%28Central%20and%20Southern%20Andes%2C%20Argentina%29.%20%3Ci%3EBasin%20Research%3C%5C%2Fi%3E%2C%20%3Ci%3E33%3C%5C%2Fi%3E%286%29%2C%203406%26%23x2013%3B3437.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fbre.12607%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fbre.12607%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Transcontinental%20retroarc%20sediment%20routing%20controlled%20by%20subduction%20geometry%20and%20climate%20change%20%28Central%20and%20Southern%20Andes%2C%20Argentina%29%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22E.%22%2C%22lastName%22%3A%22Garzanti%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22G.%22%2C%22lastName%22%3A%22Vezzoli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%22%2C%22lastName%22%3A%22Limonta%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%22%2C%22lastName%22%3A%22Sosa%22%7D%5D%2C%22abstractNote%22%3A%22Central%20Argentina%20from%20the%20Pampean%20flat-slab%20segment%20to%20northern%20Patagonia%20%2827%20degrees-41%20degrees%20S%29%20represents%20a%20classic%20example%20of%20a%20broken%20retroarc%20basin%20with%20strong%20tectonic%20and%20climatic%20control%20on%20fluvial%20sediment%20transport.%20Combined%20with%20previous%20research%20focused%20on%20coastal%20sediments%2C%20this%20actualistic%20provenance%20study%20uses%20framework%20petrography%20and%20heavy-mineral%20data%20to%20trace%20multistep%20dispersal%20of%20volcaniclastic%20detritus%20first%20eastwards%20across%20central%20Argentina%20for%20up%20to%20ca.%201%2C500%20km%20and%20next%20northwards%20for%20another%20760%20km%20along%20the%20Atlantic%20coast.%20Although%20detritus%20generated%20in%20the%20Andes%20is%20largely%20derived%20from%20mesosilicic%20volcanic%20rocks%20of%20the%20cordillera%2C%20its%20compositional%20signatures%20reflect%20different%20tectono-stratigraphic%20levels%20of%20the%20orogen%20uplifted%20along%20strike%20in%20response%20to%20varying%20subduction%20geometry%20as%20well%20as%20different%20character%20and%20crystallization%20condition%20of%20arc%20magmas%20through%20time%20and%20space.%20River%20sand%2C%20thus%2C%20changes%20from%20feldspatho-litho-quartzose%20or%20litho-feldspatho-quartzose%20in%20the%20north%2C%20where%20sedimentary%20detritus%20is%20more%20common%2C%20to%20mostly%20quartzo-feldspatho-lithic%20in%20the%20centre%20and%20to%20feldspatho-lithic%20in%20the%20south%2C%20where%20volcanic%20detritus%20is%20dominant.%20The%20transparent-heavy-mineral%20suite%20changes%20markedly%20from%20amphibole%20%3E%3E%20clinopyroxene%20%3E%20orthopyroxene%20in%20the%20north%2C%20to%20amphibole%20approximate%20to%20clinopyroxene%20approximate%20to%20orthopyroxene%20in%20the%20centre%20and%20to%20orthopyroxene%20%3E%3D%20clinopyroxene%20%3E%3E%20amphibole%20in%20the%20south.%20In%20the%20presently%20dry%20climate%2C%20fluvial%20discharge%20is%20drastically%20reduced%20to%20the%20point%20that%20even%20the%20Desaguadero%20trunk%20river%20has%20become%20endorheic%20and%20orogenic%20detritus%20is%20dumped%20in%20the%20retroarc%20basin%2C%20reworked%20by%20winds%20and%20temporarily%20accumulated%20in%20dune%20fields.%20During%20the%20Quaternary%2C%20instead%2C%20much%20larger%20amounts%20of%20water%20were%20released%20by%20melting%20of%20the%20Cordilleran%20ice%20sheet%20or%20during%20pluvial%20events.%20The%20sediment-laden%20waters%20of%20the%20Desaguadero%20and%20Colorado%20rivers%20then%20rushed%20from%20the%20tract%20of%20the%20Andes%20with%20greatest%20topographic%20and%20structural%20elevation%2C%20fostering%20alluvial%20fans%20inland%20and%20flowing%20in%20much%20larger%20valleys%20than%20today%20towards%20the%20Atlantic%20Ocean.%20Sand%20and%20gravel%20supply%20to%20the%20coast%20was%20high%20enough%20not%20only%20to%20promote%20rapid%20progradation%20of%20large%20deltaic%20lobes%20but%20also%20to%20feed%20a%20cell%20of%20littoral%20sediment%20transport%20extending%20as%20far%20north%20as%20the%20Rio%20de%20la%20Plata%20estuary.%22%2C%22date%22%3A%22Dec%202021%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1111%5C%2Fbre.12607%22%2C%22ISSN%22%3A%220950-091x%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22HCXGNCNV%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222021-06%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20McKenzie%2C%20N.%20R.%2C%20Horton%2C%20B.%20K.%2C%20Mackaman-Lofland%2C%20C.%2C%20Colleps%2C%20C.%20L.%2C%20%26amp%3B%20Stockli%2C%20D.%20F.%20%282021%29.%20Detrital%20zircon%20record%20of%20Phanerozoic%20magmatism%20in%20the%20southern%20Central%20Andes.%20%3Ci%3EGeosphere%3C%5C%2Fi%3E%2C%20%3Ci%3E17%3C%5C%2Fi%3E%283%29%2C%20876%26%23x2013%3B897.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FGes02346.1%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1130%5C%2FGes02346.1%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Detrital%20zircon%20record%20of%20Phanerozoic%20magmatism%20in%20the%20southern%20Central%20Andes%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%20R.%22%2C%22lastName%22%3A%22McKenzie%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%20L.%22%2C%22lastName%22%3A%22Colleps%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%5D%2C%22abstractNote%22%3A%22The%20spatial%20and%20temporal%20distribution%20of%20arc%20magmatism%20and%20associated%20isotopic%20variations%20provide%20insights%20into%20the%20Phanerozoic%20history%20of%20the%20western%20margin%20of%20South%20America%20during%20major%20shifts%20in%20Andean%20and%20pre-Andean%20plate%20interactions.%20We%20integrated%20detrital%20zircon%20U-Th-Pb%20and%20Hf%20isotopic%20results%20across%20continental%20magmatic%20arc%20systems%20of%20Chile%20and%20western%20Argentina%20%2828%20degrees%20S-33%20degrees%20S%29%20with%20igneous%20bedrock%20geochronologic%20and%20zircon%20Hf%20isotope%20results%20to%20define%20isotopic%20signatures%20linked%20to%20changes%20in%20continental%20margin%20processes.%20Key%20tectonic%20phases%20included%3A%20Paleozoic%20terrane%20accretion%20and%20Carboniferous%20subduction%20initiation%20during%20Gondwanide%20orogenesis%2C%20Permian-Triassic%20extensional%20collapse%2C%20Jurassic-Paleogene%20continental%20arc%20magmatism%2C%20and%20Neogene%20flat%20slab%20subduction%20during%20Andean%20shortening.%20The%20similar%20to%20550%20m.y.%20record%20of%20magmatic%20activity%20records%20spatial%20trends%20in%20magma%20composition%20associated%20with%20terrane%20boundaries.%20East%20of%2069%20degrees%20W%2C%20radiogenic%20isotopic%20signatures%20indicate%20reworked%20continental%20lithosphere%20with%20enriched%20%28evolved%29%20eHf%20values%20and%20low%20%28%3C0.65%29%20zircon%20Th%5C%2FU%20ratios%20during%20phases%20of%20early%20Paleozoic%20and%20Miocene%20shortening%20and%20lithospheric%20thickening.%20In%20contrast%2C%20the%20magmatic%20record%20west%20of%2069%20degrees%20W%20displays%20depleted%20%28juvenile%29%20eHf%20values%20and%20high%20%28%3E0.7%29%20zircon%20Th%5C%2FU%20values%20consistent%20with%20increased%20asthenospheric%20contributions%20during%20lithospheric%20thinning.%20Spatial%20constraints%20on%20Mesozoic%20to%20Cenozoic%20arc%20width%20provide%20a%20rough%20approximation%20of%20relative%20subduction%20angle%2C%20such%20that%20an%20increase%20in%20arc%20width%20reflects%20shallower%20slab%20dip.%20Comparisons%20among%20slab%20dip%20calculations%20with%20time-averaged%20eHf%20and%20Th%5C%2FU%20zircon%20results%20exhibit%20a%20clear%20trend%20of%20decreasing%20%28enriched%29%20magma%20compositions%20with%20increasing%20arc%20width%20and%20decreasing%20slab%20dip.%20Collectively%2C%20these%20data%20sets%20demonstrate%20the%20influence%20of%20subduction%20angle%20on%20the%20position%20of%20upper-plate%20magmatism%20%28including%20inboard%20arc%20advance%20and%20outboard%20arc%20retreat%29%2C%20changes%20in%20isotopic%20signatures%2C%20and%20overall%20composition%20of%20crustal%20and%20mantle%20material%20along%20the%20western%20edge%20of%20South%20America.%22%2C%22date%22%3A%22Jun%202021%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1130%5C%2FGes02346.1%22%2C%22ISSN%22%3A%221553-040x%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22BIYKG3XZ%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222020-07%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Horton%2C%20B.%20K.%2C%20McKenzie%2C%20N.%20R.%2C%20Mackaman-Lofland%2C%20C.%2C%20Stockli%2C%20D.%20F.%2C%20Ortiz%2C%20G.%2C%20%26amp%3B%20Alvarado%2C%20P.%20%282020%29.%20Neogene%20Retroarc%20Foreland%20Basin%20Evolution%2C%20Sediment%20Provenance%2C%20and%20Magmatism%20in%20Response%20to%20Flat%20Slab%20Subduction%2C%20Western%20Argentina.%20%3Ci%3ETectonics%3C%5C%2Fi%3E%2C%20%3Ci%3E39%3C%5C%2Fi%3E%287%29.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2019TC005958%2010.1029%5C%2F2019TC005958%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2019TC005958%2010.1029%5C%2F2019TC005958%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Neogene%20Retroarc%20Foreland%20Basin%20Evolution%2C%20Sediment%20Provenance%2C%20and%20Magmatism%20in%20Response%20to%20Flat%20Slab%20Subduction%2C%20Western%20Argentina%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%20R.%22%2C%22lastName%22%3A%22McKenzie%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22G.%22%2C%22lastName%22%3A%22Ortiz%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22P.%22%2C%22lastName%22%3A%22Alvarado%22%7D%5D%2C%22abstractNote%22%3A%22Understanding%20the%20effects%20of%20flat%20slab%20subduction%20on%20mountain%20building%2C%20arc%20magmatism%2C%20and%20basin%20evolution%20is%20fundamental%20to%20convergent-margin%20tectonics%2C%20with%20implications%20for%20potential%20feedbacks%20among%20geodynamic%2C%20magmatic%2C%20and%20surface%20processes.%20New%20stratigraphic%20and%20geochronological%20constraints%20on%20Cenozoic%20sedimentation%20and%20magmatism%20in%20the%20southern%20Central%20Andes%20of%20Argentina%20%2831%20degrees%20S%29%20reveal%20shifts%20in%20volcanism%2C%20foreland%5C%2Fhinterland%20basin%20development%2C%20sediment%20accumulation%2C%20and%20provenance%20as%20the%20retroarc%20region%20was%20structurally%20partitioned%20during%20slab%20flattening.%20Detrital%20zircon%20U-Pb%20age%20distributions%20from%20the%20western%20%28Calingasta%20basin%29%2C%20central%20%28Talacasto%20and%20Albarracin%20basins%29%2C%20and%20eastern%20%28Bermejo%20foreland%20basin%29%20segments%20of%20the%20retroarc%20basin%20system%20preserve%20syndepositional%20volcanism%20and%20orogenic%20unroofing%20of%20multiple%20tectonic%20provinces.%20Initial%20shortening-related%20exhumation%20of%20the%20Principal%20Cordillera%20at%2024-17%20Ma%20was%20recorded%20by%20the%20accumulation%20of%20distal%20eolian%20deposits%20bearing%20Oligocene-Eocene%20zircons%20from%20the%20Andean%20magmatic%20arc.%20The%20Calingasta%20basin%20chronicled%20volcanism%20and%20basement%20shortening%20in%20the%20Frontal%20Cordillera%20at%20similar%20to%2017-11%20Ma%2C%20as%20marked%20by%20an%20upward%20coarsening%20succession%20of%20fluvial%20to%20alluvial%20fan%20deposits%20with%20a%20sustained%20zircon%20U-Pb%20age%20component%20that%20matches%20pervasive%20Permian-Triassic%20bedrock%20in%20the%20hinterland.%20An%20similar%20to%20450%20km%20eastward%20inboard%20sweep%20of%20volcanism%20at%2011%20Ma%20coincided%20with%20the%20inception%20of%20flat%20slab%20subduction%2C%20and%20subsequent%20thin-skinned%20shortening%20in%20the%20Precordillera%20fold-thrust%20belt%20that%20exhumed%20wedge-top%20deposits%20and%20induced%20cratonward%20%28eastward%29%20advance%20of%20flexural%20subsidence%20into%20the%20Bermejo%20foreland%20basin.%20This%20foreland%20basin%20was%20structurally%20partitioned%20as%20basement%20uplifts%20of%20the%20Sierras%20Pampeanas%20transformed%20a%20fluvial%20megafan%20sediment%20routing%20network%20into%20smaller%20isolated%20alluvial%20fan%20systems%20fed%20by%20adjacent%20basement%20blocks.%22%2C%22date%22%3A%22Jul%202020%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20e2019TC005958%2010.1029%5C%2F2019TC005958%22%2C%22ISSN%22%3A%220278-7407%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22J65H3LBM%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Mackaman-Lofland%20et%20al.%22%2C%22parsedDate%22%3A%222020-03%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EMackaman-Lofland%2C%20C.%2C%20Horton%2C%20B.%20K.%2C%20Fuentes%2C%20F.%2C%20Constenius%2C%20K.%20N.%2C%20Ketcham%2C%20R.%20A.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Stockli%2C%20D.%20F.%2C%20Ammirati%2C%20J.%20B.%2C%20Alvarado%2C%20P.%2C%20%26amp%3B%20Orozco%2C%20P.%20%282020%29.%20Andean%20Mountain%20Building%20and%20Foreland%20Basin%20Evolution%20During%20Thin-%20and%20Thick-Skinned%20Neogene%20Deformation%20%2832-33%26%23xB0%3BS%29.%20%3Ci%3ETectonics%3C%5C%2Fi%3E%2C%20%3Ci%3E39%3C%5C%2Fi%3E%283%29.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2019TC005838%2010.1029%5C%2F2019TC005838%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20e2019TC005838%2010.1029%5C%2F2019TC005838%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Andean%20Mountain%20Building%20and%20Foreland%20Basin%20Evolution%20During%20Thin-%20and%20Thick-Skinned%20Neogene%20Deformation%20%2832-33%5Cu00b0S%29%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Mackaman-Lofland%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22F.%22%2C%22lastName%22%3A%22Fuentes%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20N.%22%2C%22lastName%22%3A%22Constenius%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22R.%20A.%22%2C%22lastName%22%3A%22Ketcham%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%20B.%22%2C%22lastName%22%3A%22Ammirati%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22P.%22%2C%22lastName%22%3A%22Alvarado%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22P.%22%2C%22lastName%22%3A%22Orozco%22%7D%5D%2C%22abstractNote%22%3A%22The%20southern%20Central%20Andes%20recorded%20retroarc%20shortening%2C%20basin%20evolution%2C%20and%20magmatic%20arc%20migration%20during%20Neogene%20changes%20in%20subduction.%20At%2031-33%20degrees%20S%2C%20above%20the%20modern%20flat-slab%20segment%2C%20spatial%20and%20temporal%20linkages%20between%20thin-%20and%20thick-skinned%20foreland%20shortening%2C%20basement-involved%20exhumation%20of%20the%20main%20Cordillera%2C%20and%20lower-crustal%20hinterland%20thickening%20remain%20poorly%20resolved.%20We%20integrate%20new%20geochronological%20and%20thermochronological%20data%20for%20thrust%20sheets%20and%20Neogene%20foreland%20basin%20fill%20with%20structural%2C%20sedimentological%2C%20and%20passive%20seismic%20results%20to%20reconstruct%20the%20exhumation%20history%20and%20evaluate%20potential%20geometric%20linkages%20across%20structural%20domains.%2040Ar%5C%2F39Ar%20ages%20for%20volcanic%20horizons%20and%20zircon%20U-Pb%20ages%20for%20synorogenic%20clastic%20deposits%20in%20the%20Manantiales%20Basin%20constrain%20the%20minimum%20duration%20of%20synorogenic%20sedimentation%20to%2022-14%20Ma.%20Detrital%20zircon%20age%20distributions%20record%20sequential%20unroofing%20of%20hinterland%20thrust%20sheets%20until%2015%20Ma%2C%20followed%20by%20eastward%20%28cratonward%29%20advance%20of%20the%20deformation%20front%2C%20shutoff%20of%20western%20sediment%20sources%2C%20and%20a%20shift%20from%20fluvial%20to%20alluvial%20fan%20deposition%20at%2014%20Ma.%20Apatite%20%28U-Th%29%5C%2FHe%20cooling%20ages%20confirm%20rapid%20exhumation%20of%20basement-involved%20structural%20blocks%20and%20basin%20partitioning%20by%2014-5%20Ma%2C%20consistent%20with%20the%20timing%20of%20the%20Manantiales%20facies%20and%20provenance%20shifts%20and%20a%20coeval%20%2812-9%20Ma%29%20pulse%20of%20thin-skinned%20shortening%20and%20exhumation%20previously%20identified%20in%20the%20eastern%20foreland.%20Late%20Miocene-Pliocene%20%288-2%20Ma%29%20cooling%20ages%20along%20the%20Chile-Argentina%20border%20point%20to%20hinterland%20uplift%20during%20the%20latest%20stage%20of%20Andean%20orogenesis.%20Finally%2C%20geophysical%20constraints%20on%20crustal%20architecture%20and%20low-temperature%20thermochronometry%20results%20are%20compatible%20with%20a%20hybrid%20thin-%20and%20thick-skinned%20decollement%20spanning%20retroarc%20domains.%22%2C%22date%22%3A%22Mar%202020%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20e2019TC005838%2010.1029%5C%2F2019TC005838%22%2C%22ISSN%22%3A%220278-7407%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22LTJV2F4B%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222019-11-15%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20George%2C%20S.%20W.%20M.%2C%20Hirtz%2C%20J.%20A.%2C%20Horton%2C%20B.%20K.%2C%20%26amp%3B%20Stockli%2C%20D.%20F.%20%282019%29.%20Fluvial%20and%20Eolian%20Sediment%20Mixing%20During%20Changing%20Climate%20Conditions%20Recorded%20in%20Holocene%20Andean%20Foreland%20Deposits%20From%20Argentina%20%2831-33%26%23xB0%3BS%29.%20%3Ci%3EFrontiers%20in%20Earth%20Science%3C%5C%2Fi%3E%2C%20%3Ci%3E7%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20298%2010.3389%5C%2Ffeart.2019.00298%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20298%2010.3389%5C%2Ffeart.2019.00298%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Fluvial%20and%20Eolian%20Sediment%20Mixing%20During%20Changing%20Climate%20Conditions%20Recorded%20in%20Holocene%20Andean%20Foreland%20Deposits%20From%20Argentina%20%2831-33%5Cu00b0S%29%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22S.%20W.%20M.%22%2C%22lastName%22%3A%22George%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%20A.%22%2C%22lastName%22%3A%22Hirtz%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%5D%2C%22abstractNote%22%3A%22Continental%20drainage%20systems%20archive%20complex%20records%20of%20rock%20uplift%2C%20source%20area%20relief%2C%20precipitation%2C%20glaciation%2C%20and%20carbon%20cyclicity%20driven%20largely%20by%20tectonics%20and%20climate.%20Significant%20progress%20has%20been%20made%20in%20linking%20such%20external%20environmental%20forcings%20to%20the%20geomorphic%20expression%20of%20landscapes%20and%20the%20stratigraphic%20record%20of%20depositional%20basins%20in%20coastal%20and%20offshore%20areas.%20However%2C%20there%20are%20large%20uncertainties%20in%20the%20degree%20to%20which%20sediment%20dispersal%20processes%20can%20modify%20signals%20between%20the%20erosional%20sources%20and%20the%20depositional%20sinks.%20We%20investigate%20a%20Holocene%20sediment%20transfer%20zone%20with%20contrasting%20fluvial%20and%20eolian%20sediment%20transport%20mechanisms%20to%20understand%20how%20river%20and%20wind%20processes%20impact%20the%20propagation%20of%20environmental%20signals%20in%20continental-scale%20drainage%20systems.%20To%20quantify%20these%20processes%2C%20we%20employ%20sediment%20fingerprinting%20methods%20for%20unconsolidated%20sand%20samples%20%28detrital%20zircon%20U-Pb%20geochronology%29%2C%20incorporate%20sediment%20mixing%20models%2C%20and%20correlate%20the%20findings%20with%20the%20regional%20geologic%20and%20geomorphic%20framework.%20Three%20contrasting%20source%20regions%20deliver%20sediment%20to%20the%20Andean%20foreland%3A%20volcanic%20rocks%20of%20the%20Frontal%20Cordillera%2C%20sedimentary%20rocks%20of%20the%20Precordillera%2C%20and%20metamorphic%20basement%20of%20the%20Sierras%20Pampeanas.%20Although%20all%20samples%20of%20Holocene%20eolian%20dunes%20accurately%20record%20sediment%20input%20from%20three%20fluvial%20source%20regions%2C%20spatial%20variations%20in%20U-Pb%20results%20are%20consistent%20with%20north-directed%20paleowinds%2C%20whereby%20river%20sediments%20from%20Frontal%20Cordillera%20sources%20are%20transported%20northward%20and%20progressively%20mixed%20with%20river%20sediments%20from%20Precordillera%20and%20Sierras%20Pampeanas%20sources.%20In%20contrast%2C%20samples%20of%20modern%20rivers%20show%20progressive%20southward%20%28downstream%29%20mixing%20along%20a%20large%20axial%20fluvial%20system.%20Sediment%20mixing%20induced%20by%20eolian%20transport%20and%20reworking%20of%20various%20sources%20is%20likely%20a%20critical%2C%20climate-modulated%20process%20in%20the%20propagation%20of%20environmental%20signals%2C%20potentially%20involving%20the%20aliasing%20of%20tectonic%20signals%2C%20local%20storage%20and%20recycling%20of%20synorogenic%20river%20sediment%2C%20and%20cyclical%20patterns%20of%20sediment%20starvation%20and%20delivery%20to%20distal%20zones%20of%20accumulation.%22%2C%22date%22%3A%22Nov%2015%202019%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20298%2010.3389%5C%2Ffeart.2019.00298%22%2C%22ISSN%22%3A%22%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A55Z%22%7D%7D%2C%7B%22key%22%3A%22DEUZ4GC2%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Sickmann%20et%20al.%22%2C%22parsedDate%22%3A%222019-10-01%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3ESickmann%2C%20Z.%20T.%2C%20Chheda%2C%20T.%20D.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Thomson%2C%20K.%20D.%2C%20Paull%2C%20C.%20K.%2C%20%26amp%3B%20Graham%2C%20S.%20A.%20%282019%29.%20Using%20provenance%20analysis%20in%20an%20Anthropocene%20natural%20laboratory.%20%3Ci%3EQuaternary%20Science%20Reviews%3C%5C%2Fi%3E%2C%20%3Ci%3E221%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20105890%2010.1016%5C%2Fj.quascirev.2019.105890%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2FARTN%20105890%2010.1016%5C%2Fj.quascirev.2019.105890%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Using%20provenance%20analysis%20in%20an%20Anthropocene%20natural%20laboratory%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Z.%20T.%22%2C%22lastName%22%3A%22Sickmann%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20D.%22%2C%22lastName%22%3A%22Chheda%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20D.%22%2C%22lastName%22%3A%22Thomson%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%20K.%22%2C%22lastName%22%3A%22Paull%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22S.%20A.%22%2C%22lastName%22%3A%22Graham%22%7D%5D%2C%22abstractNote%22%3A%22Globally%2C%20anthropogenic%20perturbations%20to%20sediment%20dispersal%20systems%20produce%20detrital%20signals%20that%20are%20evident%20in%20the%20recent%20sedimentary%20record.%20We%20review%20the%20study%20of%20anthropogenic%20perturbations%20to%20sediment%20dispersal%20systems%20from%20the%20perspective%20of%20detrital%20signals%20and%20discuss%20the%20use%20of%20provenance%20analysis%20in%20Anthropocene%20sedimentology.%20Anthropocene%20provenance%20analysis%20is%20illustrated%20by%20a%20case%20study%20from%20the%20Monterey%20Bay%20Sediment%20Dispersal%20System%20%28MBDS%29%20of%20coastal%20and%20offshore%20central%20California%2C%20U.S.A.%20The%20MBDS%20records%20two%20phases%20of%20alterations%20to%20sediment%20flux%2C%20an%20early%20increase%20in%20fine%20flux%20recognized%20in%20increased%20sedimentation%20rates%20and%20a%20later%20decrease%20in%20coarse%20flux%20recognized%20in%20detrital%20provenance%20signatures.%20Results%20from%20the%20MBDS%20suggest%20that%20a%20multi-methodological%20approaches%20employing%20provenance%20analysis%2C%20and%20detailed%2C%20short-timescale%20%2810%282%29-10%284%29%20yr%29%20depositional%20chronology%20markers%20combined%20with%20the%20study%20of%20other%20Anthropocene%20indicators%20like%20the%20introduction%20of%20non-natural%20detritus%20are%20valuable%20tools%20for%20describing%20natural%20sedimentary%20processes%20in%20addition%20to%20human%20alterations%20to%20natural%20systems.%20The%20recognition%20and%20description%20of%20such%20perturbations%20to%20sediment%20supply%20is%20increasingly%20recognized%20as%20an%20important%20variable%20in%20understanding%20the%20effects%20of%20human-driven%20landscape%20alteration%2C%20particularly%20in%20the%20face%20of%20a%20changing%20climate.%20The%20broad%20concepts%20and%20approach%20outlined%20in%20this%20study%20provide%20tools%20that%20can%20extend%20environmental%20observations%20past%20the%20period%20of%20historical%20record%20and%20can%20be%20used%20to%20understand%20past%2C%20and%20predict%20future%2C%20impacts%20of%20altered%20sediment%20flux%20in%20response%20to%20drivers%20like%20climate%20change%20and%20sea%20level%20rise.%20%28C%29%202019%20Elsevier%20Ltd.%20All%20rights%20reserved.%22%2C%22date%22%3A%22Oct%201%202019%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%22ARTN%20105890%2010.1016%5C%2Fj.quascirev.2019.105890%22%2C%22ISSN%22%3A%220277-3791%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A55Z%22%7D%7D%2C%7B%22key%22%3A%227MLH5FFR%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Odlum%20et%20al.%22%2C%22parsedDate%22%3A%222019-08-20%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EOdlum%2C%20M.%20L.%2C%20Stockli%2C%20D.%20F.%2C%20%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Thomson%2C%20K.%20D.%2C%20Clark%2C%20J.%2C%20Puigdef%26%23xE1%3Bbregas%2C%20C.%2C%20%26amp%3B%20Fildani%2C%20A.%20%282019%29.%20Tectonic%20and%20sediment%20provenance%20evolution%20of%20the%20South%20Eastern%20Pyrenean%20foreland%20basins%20during%20rift%20margin%20inversion%20and%20orogenic%20uplift.%20%3Ci%3ETectonophysics%3C%5C%2Fi%3E%2C%20%3Ci%3E765%3C%5C%2Fi%3E%2C%20226%26%23x2013%3B248.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.tecto.2019.05.008%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.tecto.2019.05.008%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Tectonic%20and%20sediment%20provenance%20evolution%20of%20the%20South%20Eastern%20Pyrenean%20foreland%20basins%20during%20rift%20margin%20inversion%20and%20orogenic%20uplift%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20L.%22%2C%22lastName%22%3A%22Odlum%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20D.%22%2C%22lastName%22%3A%22Thomson%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%22%2C%22lastName%22%3A%22Clark%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22C.%22%2C%22lastName%22%3A%22Puigdef%5Cu00e1bregas%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22A.%22%2C%22lastName%22%3A%22Fildani%22%7D%5D%2C%22abstractNote%22%3A%22The%20Cretaceous%20to%20Oligocene%20detrital%20record%20in%20the%20southern%20Eastern%20Pyrenees%20is%20utilized%20to%20address%20the%20degree%20to%20which%20precursor%20basin%20architecture%20and%20hyper-extensional%20rift%20structures%20impacted%20subsequent%20sedimentary%20provenance%20and%20dispersal%20systems%20and%20foreland%20basin%20evolution.%20This%20study%20presents%20new%20isotopic%20provenance%20analysis%20of%20detrital%20zircon%20U-Pb%20and%20%28U-Th%29%5C%2FHe%20double-dating%2C%20and%20detrital%20rutile%20U-Pb%20and%20trace%20element%20geochemistry%20to%20track%20sediment%20provenance%20evolution.%20Late%20Cretaceous-Paleocene%20sediments%20show%20zircon%20with%20dominantly%20Variscan%20U-Pb%20and%20Jurassic-Early%20Cretaceous%20ZHe%20cooling%20ages%20that%20are%20derived%20from%20southeastern%20Catalan%20Coastal%20Ranges%20and%20eastern%20Corsica-Sardinia%20regions%2C%20and%20localized%20structural%20inversion%20along%20inherited%20Mesozoic%20extensional%20faults%20and%20erosional%20recycling%20of%20syn-rift%20sediments.%20Eocene%20deposits%20have%20multimodal%20U-Pb%20ages%20that%20stratigraphically%20upsection%20change%20to%20unimodal%20Variscan%20ages%2C%20with%20the%20appearance%20and%20upsection%20increase%20in%20Pyrenean%20ZHe%20ages%2C%20and%20increase%20in%20Variscan%20aged%20detrital%20rutile%20that%20record%20a%20significant%20shift%20in%20sediment%20source%20area%20to%20northern%20sources%20recording%20exhumation%20and%20unroofing%20of%20the%20Axial%20Zone%20Paleozoic%20basement%20sources%2C%20and%20development%20of%20new%20ramp-flat%20style%20structures%20in%20the%20Southern%20Pyrenean%20Zone%20fold-thrust%20belt.%20During%20the%20Oligocene%2C%20incipient%20foreland%20basin%20deposits%20were%20cannibalized%20and%20recycled%20into%20the%20foreland%20basin%20as%20thrusting%20advanced%20toward%20the%20foreland.%20The%20Eastern%20Pyrenean%20foreland%20basin%20records%20a%20different%20provenance%20history%20from%20Central%20Pyrenean%20Tremp%20Basin%2C%20suggesting%20the%20basins%20were%20segmented%20throughout%20the%20Late%20Cretaceous%20to%20Oligocene%2C%20while%20the%20Ripoll%20and%20Ager%20basins%20appear%20to%20have%20shared%20similar%20source%20areas.%20The%20sediment%20provenance%20evolution%20coupled%20with%20Pyrenean%20fault%20activity%20and%20shortening%20rates%2C%20hinterland%20exhumation%2C%20foreland%20basin%20subsidence%2C%20and%20climate%20proxies%20presents%20a%20detailed%20dataset%20to%20understand%20these%20relationships%20within%20the%20Eastern%20Pyrenean%20orogenic%20system%20and%20highlight%20the%20dominant%20control%20precursor%20basins%20and%20structural%20inheritance%20has%20on%20the%20subsequent%20fold-thrust%20belts%20and%20foreland%20basin%20evolution.%22%2C%22date%22%3A%22Aug%2020%202019%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1016%5C%2Fj.tecto.2019.05.008%22%2C%22ISSN%22%3A%220040-1951%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%2C%228MGFHE4Z%22%5D%2C%22dateModified%22%3A%222024-02-23T23%3A13%3A55Z%22%7D%7D%2C%7B%22key%22%3A%22VYWMBGJE%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Capaldi%20et%20al.%22%2C%22parsedDate%22%3A%222017-12-01%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3ECapaldi%3C%5C%2Fstrong%3E%2C%20T.%20N.%2C%20Horton%2C%20B.%20K.%2C%20McKenzie%2C%20N.%20R.%2C%20Stockli%2C%20D.%20F.%2C%20%26amp%3B%20Odium%2C%20M.%20L.%20%282017%29.%20Sediment%20provenance%20in%20contractional%20orogens%3A%20The%20detrital%20zircon%20record%20from%20modern%20rivers%20in%20the%20Andean%20fold-thrust%20belt%20and%20foreland%20basin%20of%20western%20Argentina.%20%3Ci%3EEarth%20and%20Planetary%20Science%20Letters%3C%5C%2Fi%3E%2C%20%3Ci%3E479%3C%5C%2Fi%3E%2C%2083%26%23x2013%3B97.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.epsl.2017.09.001%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1016%5C%2Fj.epsl.2017.09.001%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Sediment%20provenance%20in%20contractional%20orogens%3A%20The%20detrital%20zircon%20record%20from%20modern%20rivers%20in%20the%20Andean%20fold-thrust%20belt%20and%20foreland%20basin%20of%20western%20Argentina%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22T.%20N.%22%2C%22lastName%22%3A%22Capaldi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%20K.%22%2C%22lastName%22%3A%22Horton%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%20R.%22%2C%22lastName%22%3A%22McKenzie%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22D.%20F.%22%2C%22lastName%22%3A%22Stockli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20L.%22%2C%22lastName%22%3A%22Odium%22%7D%5D%2C%22abstractNote%22%3A%22This%20study%20analyzes%20detrital%20zircon%20U-Pb%20age%20populations%20from%20Andean%20rivers%20to%20assess%20whether%20active%20synorogenic%20sedimentation%20accurately%20records%20proportional%20contributions%20from%20varied%20bedrock%20source%20units%20across%20different%20drainage%20areas.%20Samples%20of%20modern%20river%20sand%20were%20collected%20from%20west-central%20Argentina%20%2828-33%20degrees%20S%29%2C%20where%20the%20Andes%20are%20characterized%20by%20active%20uplift%20and%20deposition%20in%20diverse%20contractional%20provinces%2C%20including%20%281%29%20hinterland%2C%20%282%29%20wedge-top%2C%20%283%29%20proximal%20foreland%2C%20and%20%284%29%20distal%20broken%20foreland%20basin%20settings.%20Potential%20controls%20on%20sediment%20provenance%20were%20evaluated%20by%20comparing%20river%20U-Pb%20age%20distributions%20with%20predicted%20age%20spectra%20generated%20by%20a%20sediment%20mixing%20model%20weighted%20by%20relative%20catchment%20exposure%20%28outcrop%29%20areas%20for%20different%20source%20units.%20Several%20statistical%20measures%20%28similarity%2C%20likeness%2C%20and%20cross-correlation%29%20are%20employed%20to%20compare%20how%20well%20the%20area-weighted%20model%20predicts%20modern%20river%20age%20populations.%20%281%29%20Hinterland%20basin%20provenance%20is%20influenced%20by%20local%20relief%20generated%20along%20thrust-bounded%20ranges%20and%20high%20zircon%20fertility%20of%20exposed%20crystalline%20basement.%20%282%29%20Wedge-top%20%28piggyback%29%20basin%20provenance%20is%20controlled%20by%20variable%20lithologic%20durability%20among%20thrust%20belt%20bedrock%20sources%20and%20recycled%20basin%20sediments.%20%283%29%20Proximal%20foreland%20%28foredeep%29%20basin%20provenance%20of%20rivers%20and%20fluvial%20megafans%20accurately%20reflect%20regional%20bedrock%20distributions%2C%20with%20limited%20effects%20of%20zircon%20fertility%20and%20lithologic%20durability%20in%20large%20%28%3E20%2C000%20km%282%29%29%20second-order%20drainage%20systems.%20%284%29%20In%20distal%20broken%20segments%20of%20the%20foreland%20basin%2C%20regional%20provenance%20signatures%20from%20thrust-belt%20and%20hinterland%20areas%20are%20diluted%20by%20local%20contributions%20from%20foreland%20basement-cored%20uplifts.%20%28C%29%202017%20Elsevier%20B.V.%20All%20rights%20reserved.%22%2C%22date%22%3A%22Dec%201%202017%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1016%5C%2Fj.epsl.2017.09.001%22%2C%22ISSN%22%3A%220012-821x%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22BGC9F53I%22%2C%228MGFHE4Z%22%5D%2C%22dateModified%22%3A%222024-04-12T20%3A11%3A54Z%22%7D%7D%5D%7D

Odlum, M. L., Capaldi, T. N., Thomson, K. D., & Stockli, D. F. (2024). Tracking cycles of Phanerozoic opening and closing of ocean basins using detrital rutile and zircon geochronology and geochemistry. Geology. https://doi.org/10.1130/G51826.1

Starck, D., Capaldi, T. N., Fuentes, F., & Horton, B. K. (2024). Tectonic and climatic significance of Oligocene-Miocene eolian sandstones in the Andean foreland basin of Argentina. Journal of South American Earth Sciences, 134, 20. https://doi.org/10.1016/j.jsames.2023.104758

Plonka, Z. C., Capaldi, T. N., Odlum, M. L., Mackaman-Lofland, C., Ortiz, G., & Alvarado, P. (2023). Along-strike tectonic evolution of the Neogene Bermejo foreland basin and Eastern Precordillera thrust front, Argentina (30-32°S). Journal of South American Earth Sciences, 129. https://doi.org/10.1016/j.jsames.2023.104521

Akciz, S. O., Ludwig, L. G., Arrowsmith, R. J., Capaldi, T. N., & Rhodes, E. J. (2023). Channel Incision Ages to the Rescue: An Improved Age for the Penultimate Earthquake That Ruptured the Carrizo Section of the South- Central San Andreas Fault. Bulletin of the Seismological Society of America, 113(2), 877–887. https://doi.org/10.1785/0120220189

Horton, B. K., Capaldi, T. N., Mackaman-Lofland, C., Perez, N. D., Bush, M. A., Fuentes, F., & Constenius, K. N. (2022). Broken foreland basins and the influence of subduction dynamics, tectonic inheritance, and mechanical triggers. Earth-Science Reviews, 234. https://doi.org/ARTN 104193 10.1016/j.earscirev.2022.104193

Capaldi, T. N., Odlum, M. L., Curry, M. E., & Stockli, D. F. (2022). Variable thermal histories across the Pyrenees orogen recorded in modern river sand detrital geo-/thermochronology and PECUBE thermokinematic modelling. Basin Research, 34(5), 1781–1806. https://doi.org/10.1111/bre.12685

Horton, B. K., Capaldi, T. N., & Perez, N. D. (2022). The role of flat slab subduction, ridge subduction, and tectonic inheritance in Andean deformation. Geology, 50(9), 1007–1012. https://doi.org/10.1130/G50094.1

Garzanti, E., Capaldi, T., Tripaldi, A., Zarate, M., Limonta, M., & Vezzoli, G. (2022). Andean retroarc-basin dune fields and Pampean Sand Sea (Argentina): Provenance and drainage changes driven by tectonics and climate. Earth-Science Reviews, 231. https://doi.org/ARTN 104077 10.1016/j.earscirev.2022.104077

Capaldi, T. N., Rittenour, T. M., & Nelson, M. S. (2022). Downstream changes in quartz OSL sensitivity in modern river sand reflects sediment source variability: Case studies from Rocky Mountain and Andean rivers. Quaternary Geochronology, 71. https://doi.org/ARTN 101317 10.1016/j.quageo.2022.101317

Mackaman-Lofland, C., Horton, B. K., Ketcham, R. A., McQuarrie, N., Fosdick, J. C., Fuentes, F., Constenius, K. N., Capaldi, T. N., Stockli, D. F., & Alvarado, P. (2022). Causes of Variable Shortening and Tectonic Subsidence During Changes in Subduction: Insights From Flexural Thermokinematic Modeling of the Neogene Southern Central Andes (28-30°S). Tectonics, 41(8). https://doi.org/ARTN e2022TC007334 10.1029/2022TC007334

Garzanti, E., Capaldi, T., Vezzoli, G., Limonta, M., & Sosa, N. (2021). Transcontinental retroarc sediment routing controlled by subduction geometry and climate change (Central and Southern Andes, Argentina). Basin Research, 33(6), 3406–3437. https://doi.org/10.1111/bre.12607

Capaldi, T. N., McKenzie, N. R., Horton, B. K., Mackaman-Lofland, C., Colleps, C. L., & Stockli, D. F. (2021). Detrital zircon record of Phanerozoic magmatism in the southern Central Andes. Geosphere, 17(3), 876–897. https://doi.org/10.1130/Ges02346.1

Capaldi, T. N., Horton, B. K., McKenzie, N. R., Mackaman-Lofland, C., Stockli, D. F., Ortiz, G., & Alvarado, P. (2020). Neogene Retroarc Foreland Basin Evolution, Sediment Provenance, and Magmatism in Response to Flat Slab Subduction, Western Argentina. Tectonics, 39(7). https://doi.org/ARTN e2019TC005958 10.1029/2019TC005958

Mackaman-Lofland, C., Horton, B. K., Fuentes, F., Constenius, K. N., Ketcham, R. A., Capaldi, T. N., Stockli, D. F., Ammirati, J. B., Alvarado, P., & Orozco, P. (2020). Andean Mountain Building and Foreland Basin Evolution During Thin- and Thick-Skinned Neogene Deformation (32-33°S). Tectonics, 39(3). https://doi.org/ARTN e2019TC005838 10.1029/2019TC005838

Capaldi, T. N., George, S. W. M., Hirtz, J. A., Horton, B. K., & Stockli, D. F. (2019). Fluvial and Eolian Sediment Mixing During Changing Climate Conditions Recorded in Holocene Andean Foreland Deposits From Argentina (31-33°S). Frontiers in Earth Science, 7. https://doi.org/ARTN 298 10.3389/feart.2019.00298

Sickmann, Z. T., Chheda, T. D., Capaldi, T. N., Thomson, K. D., Paull, C. K., & Graham, S. A. (2019). Using provenance analysis in an Anthropocene natural laboratory. Quaternary Science Reviews, 221. https://doi.org/ARTN 105890 10.1016/j.quascirev.2019.105890

Odlum, M. L., Stockli, D. F., Capaldi, T. N., Thomson, K. D., Clark, J., Puigdefábregas, C., & Fildani, A. (2019). Tectonic and sediment provenance evolution of the South Eastern Pyrenean foreland basins during rift margin inversion and orogenic uplift. Tectonophysics, 765, 226–248. https://doi.org/10.1016/j.tecto.2019.05.008

Capaldi, T. N., Horton, B. K., McKenzie, N. R., Stockli, D. F., & Odium, M. L. (2017). Sediment provenance in contractional orogens: The detrital zircon record from modern rivers in the Andean fold-thrust belt and foreland basin of western Argentina. Earth and Planetary Science Letters, 479, 83–97. https://doi.org/10.1016/j.epsl.2017.09.001