New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation

We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital...
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Autor*in:	Zhou, Renjie [verfasserIn] Schoenbohm, Lindsay M Sobel, Edward R Davis, Donald W Glodny, Johannes

Format:	Artikel
Sprache:	Englisch

Erschienen:	2016

Rechteinformationen:	Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc.

Schlagwörter:	Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation

Übergeordnetes Werk:	Enthalten in: Geological Society of America bulletin - Boulder, Colo. [u.a.] : Geological Society of America, 1890, 129(2016), 1-2, Seite 152
Übergeordnetes Werk:	volume:129 ; year:2016 ; number:1-2 ; pages:152

Links:	Volltext Link aufrufen

DOI / URN:	10.1130/B31384.1

Katalog-ID:	OLC1988317460

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520			\|a We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene.
540			\|a Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc.
650		4	\|a Natural history
650		4	\|a Plateaus
650		4	\|a Sedimentary geology
650		4	\|a Rocks
650		4	\|a Magma
650		4	\|a Sediments
650		4	\|a Deformation
700	1		\|a Schoenbohm, Lindsay M \|4 oth
700	1		\|a Sobel, Edward R \|4 oth
700	1		\|a Davis, Donald W \|4 oth
700	1		\|a Glodny, Johannes \|4 oth
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allfields	10.1130/B31384.1 doi PQ20170206 (DE-627)OLC1988317460 (DE-599)GBVOLC1988317460 (PRQ)c1449-16359a7f17c56f0ad27a51f1cddaf02d707b646221f39a754867f74739071aef0 (KEY)0093391020160000129000100152newconstraintsonorogenicmodelsofthesoutherncentral DE-627 ger DE-627 rakwb eng 550 DNB Zhou, Renjie verfasserin aut New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene. Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc. Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation Schoenbohm, Lindsay M oth Sobel, Edward R oth Davis, Donald W oth Glodny, Johannes oth Enthalten in Geological Society of America bulletin Boulder, Colo. [u.a.] : Geological Society of America, 1890 129(2016), 1-2, Seite 152 (DE-627)129067199 (DE-600)1351-1 (DE-576)014398621 0016-7606 nnns volume:129 year:2016 number:1-2 pages:152 http://dx.doi.org/10.1130/B31384.1 Volltext http://search.proquest.com/docview/1856103786 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4323 AR 129 2016 1-2 152
spelling	10.1130/B31384.1 doi PQ20170206 (DE-627)OLC1988317460 (DE-599)GBVOLC1988317460 (PRQ)c1449-16359a7f17c56f0ad27a51f1cddaf02d707b646221f39a754867f74739071aef0 (KEY)0093391020160000129000100152newconstraintsonorogenicmodelsofthesoutherncentral DE-627 ger DE-627 rakwb eng 550 DNB Zhou, Renjie verfasserin aut New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene. Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc. Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation Schoenbohm, Lindsay M oth Sobel, Edward R oth Davis, Donald W oth Glodny, Johannes oth Enthalten in Geological Society of America bulletin Boulder, Colo. [u.a.] : Geological Society of America, 1890 129(2016), 1-2, Seite 152 (DE-627)129067199 (DE-600)1351-1 (DE-576)014398621 0016-7606 nnns volume:129 year:2016 number:1-2 pages:152 http://dx.doi.org/10.1130/B31384.1 Volltext http://search.proquest.com/docview/1856103786 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4323 AR 129 2016 1-2 152
allfields_unstemmed	10.1130/B31384.1 doi PQ20170206 (DE-627)OLC1988317460 (DE-599)GBVOLC1988317460 (PRQ)c1449-16359a7f17c56f0ad27a51f1cddaf02d707b646221f39a754867f74739071aef0 (KEY)0093391020160000129000100152newconstraintsonorogenicmodelsofthesoutherncentral DE-627 ger DE-627 rakwb eng 550 DNB Zhou, Renjie verfasserin aut New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene. Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc. Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation Schoenbohm, Lindsay M oth Sobel, Edward R oth Davis, Donald W oth Glodny, Johannes oth Enthalten in Geological Society of America bulletin Boulder, Colo. [u.a.] : Geological Society of America, 1890 129(2016), 1-2, Seite 152 (DE-627)129067199 (DE-600)1351-1 (DE-576)014398621 0016-7606 nnns volume:129 year:2016 number:1-2 pages:152 http://dx.doi.org/10.1130/B31384.1 Volltext http://search.proquest.com/docview/1856103786 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4323 AR 129 2016 1-2 152
allfieldsGer	10.1130/B31384.1 doi PQ20170206 (DE-627)OLC1988317460 (DE-599)GBVOLC1988317460 (PRQ)c1449-16359a7f17c56f0ad27a51f1cddaf02d707b646221f39a754867f74739071aef0 (KEY)0093391020160000129000100152newconstraintsonorogenicmodelsofthesoutherncentral DE-627 ger DE-627 rakwb eng 550 DNB Zhou, Renjie verfasserin aut New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene. Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc. Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation Schoenbohm, Lindsay M oth Sobel, Edward R oth Davis, Donald W oth Glodny, Johannes oth Enthalten in Geological Society of America bulletin Boulder, Colo. [u.a.] : Geological Society of America, 1890 129(2016), 1-2, Seite 152 (DE-627)129067199 (DE-600)1351-1 (DE-576)014398621 0016-7606 nnns volume:129 year:2016 number:1-2 pages:152 http://dx.doi.org/10.1130/B31384.1 Volltext http://search.proquest.com/docview/1856103786 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4323 AR 129 2016 1-2 152
allfieldsSound	10.1130/B31384.1 doi PQ20170206 (DE-627)OLC1988317460 (DE-599)GBVOLC1988317460 (PRQ)c1449-16359a7f17c56f0ad27a51f1cddaf02d707b646221f39a754867f74739071aef0 (KEY)0093391020160000129000100152newconstraintsonorogenicmodelsofthesoutherncentral DE-627 ger DE-627 rakwb eng 550 DNB Zhou, Renjie verfasserin aut New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene. Nutzungsrecht: © COPYRIGHT 2017 Geological Society of America, Inc. Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation Schoenbohm, Lindsay M oth Sobel, Edward R oth Davis, Donald W oth Glodny, Johannes oth Enthalten in Geological Society of America bulletin Boulder, Colo. [u.a.] : Geological Society of America, 1890 129(2016), 1-2, Seite 152 (DE-627)129067199 (DE-600)1351-1 (DE-576)014398621 0016-7606 nnns volume:129 year:2016 number:1-2 pages:152 http://dx.doi.org/10.1130/B31384.1 Volltext http://search.proquest.com/docview/1856103786 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4323 AR 129 2016 1-2 152
language	English
source	Enthalten in Geological Society of America bulletin 129(2016), 1-2, Seite 152 volume:129 year:2016 number:1-2 pages:152
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author	Zhou, Renjie
spellingShingle	Zhou, Renjie ddc 550 misc Natural history misc Plateaus misc Sedimentary geology misc Rocks misc Magma misc Sediments misc Deformation New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation
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topic_title	550 DNB New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation Natural history Plateaus Sedimentary geology Rocks Magma Sediments Deformation
topic	ddc 550 misc Natural history misc Plateaus misc Sedimentary geology misc Rocks misc Magma misc Sediments misc Deformation
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title	New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation
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title_full	New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation
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title_sort	new constraints on orogenic models of the southern central andean plateau: cenozoic basin evolution and bedrock exhumation
title_auth	New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation
abstract	We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene.
abstractGer	We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene.
abstract_unstemmed	We present a multidisciplinary study that constrains the development history of the southern part of the Central Andean Plateau, a prototypical noncollisional orogenic system. In the Antofagasta de la Sierra region of NW Argentina, data from sedimentary geology, sandstone modal composition, detrital zircon U-Pb geochronology, and apatite fission-track and (U-Th-Sm)/He thermochronology indicate that sediments accumulated in the late Eocene to early Oligocene, with a maximum depositional age of ca. 39-38 Ma provided by the youngest detrital zircon U-Pb dates. Provenance data, including paleocurrent indicators, sandstone modal composition, and detrital zircon U-Pb ages, point to prevailing western sources, including the Sierra de Quebrada Honda (a proximal source), the Ordovician to Late Cambrian Famatinian magmatic arc in western Argentina and Chile (a distal source), and the Permian-Triassic plutonic and volcanic rocks in coastal Chile (a distal source). Along the western basin margin, these strata were deformed by a basement-involved thrust fault that was active at ca. 25-20 Ma, as constrained by apatite fission-track and (U-Th-Sm)/He data. Analysis of new and existing U-Pb geochronologic data from both detrital and basement samples across the Puna suggests that the Sierra Laguna Blanca, a major mountain range in the southern Puna, remained buried during the late Eocene to early Oligocene. Our multidisciplinary data indicate that the southern Central Andean Plateau may have hosted a regional basin primarily formed by lithospheric flexure during the late Eocene to early Oligocene. Furthermore, this study refines the history of basin compartmentalization and exhumation of the major mountain ranges in the southern Puna, revealing propagation of deformation from the west to east, starting as early as the late Eocene and continuing to the mid-late Miocene.
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title_short	New constraints on orogenic models of the southern Central Andean Plateau: Cenozoic basin evolution and bedrock exhumation
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