Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina
The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedg...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Payrola, Patricio [verfasserIn] del Papa, Cecilia [verfasserIn] Aramayo, Alejandro [verfasserIn] Pingel, Heiko [verfasserIn] Hongn, Fernando [verfasserIn] Sobel, Edward R. [verfasserIn] Zeilinger, Gerold [verfasserIn] Strecker, Manfred R. [verfasserIn] Zapata, Sebastian [verfasserIn] Cottle, John [verfasserIn] Salado Paz, Natalia [verfasserIn] Glodny, Johannes [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation |
|---|
| Übergeordnetes Werk: |
Enthalten in: Tectonophysics - Amsterdam [u.a.] : Elsevier, 1964, 776 |
|---|---|
| Übergeordnetes Werk: |
volume:776 |
| DOI / URN: |
10.1016/j.tecto.2019.228276 |
|---|
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ELV003659666 |
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| 520 | |a The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. | ||
| 650 | 4 | |a Central Andes | |
| 650 | 4 | |a NW Argentina | |
| 650 | 4 | |a Unconformities | |
| 650 | 4 | |a Orogenic Wedge | |
| 650 | 4 | |a U-Pb zircon geochronology | |
| 650 | 4 | |a Apatite U-Th/He thermochronology | |
| 650 | 4 | |a Eocene-to-Miocene multiple fault reactivations | |
| 650 | 4 | |a Basement-involved faults and non-systematic propagation of deformation | |
| 650 | 4 | |a Structural geology | |
| 650 | 4 | |a U-Pb geochronology | |
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| 700 | 1 | |a Hongn, Fernando |e verfasserin |4 aut | |
| 700 | 1 | |a Sobel, Edward R. |e verfasserin |4 aut | |
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| 700 | 1 | |a Salado Paz, Natalia |e verfasserin |4 aut | |
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10.1016/j.tecto.2019.228276 doi (DE-627)ELV003659666 (ELSEVIER)S0040-1951(19)30391-9 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Payrola, Patricio verfasserin (orcid)0000-0001-8697-5914 aut Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera del Papa, Cecilia verfasserin aut Aramayo, Alejandro verfasserin aut Pingel, Heiko verfasserin aut Hongn, Fernando verfasserin aut Sobel, Edward R. verfasserin aut Zeilinger, Gerold verfasserin aut Strecker, Manfred R. verfasserin aut Zapata, Sebastian verfasserin aut Cottle, John verfasserin aut Salado Paz, Natalia verfasserin aut Glodny, Johannes verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 776 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:776 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 776 |
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10.1016/j.tecto.2019.228276 doi (DE-627)ELV003659666 (ELSEVIER)S0040-1951(19)30391-9 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Payrola, Patricio verfasserin (orcid)0000-0001-8697-5914 aut Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera del Papa, Cecilia verfasserin aut Aramayo, Alejandro verfasserin aut Pingel, Heiko verfasserin aut Hongn, Fernando verfasserin aut Sobel, Edward R. verfasserin aut Zeilinger, Gerold verfasserin aut Strecker, Manfred R. verfasserin aut Zapata, Sebastian verfasserin aut Cottle, John verfasserin aut Salado Paz, Natalia verfasserin aut Glodny, Johannes verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 776 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:776 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 776 |
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10.1016/j.tecto.2019.228276 doi (DE-627)ELV003659666 (ELSEVIER)S0040-1951(19)30391-9 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Payrola, Patricio verfasserin (orcid)0000-0001-8697-5914 aut Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera del Papa, Cecilia verfasserin aut Aramayo, Alejandro verfasserin aut Pingel, Heiko verfasserin aut Hongn, Fernando verfasserin aut Sobel, Edward R. verfasserin aut Zeilinger, Gerold verfasserin aut Strecker, Manfred R. verfasserin aut Zapata, Sebastian verfasserin aut Cottle, John verfasserin aut Salado Paz, Natalia verfasserin aut Glodny, Johannes verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 776 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:776 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 776 |
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10.1016/j.tecto.2019.228276 doi (DE-627)ELV003659666 (ELSEVIER)S0040-1951(19)30391-9 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Payrola, Patricio verfasserin (orcid)0000-0001-8697-5914 aut Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera del Papa, Cecilia verfasserin aut Aramayo, Alejandro verfasserin aut Pingel, Heiko verfasserin aut Hongn, Fernando verfasserin aut Sobel, Edward R. verfasserin aut Zeilinger, Gerold verfasserin aut Strecker, Manfred R. verfasserin aut Zapata, Sebastian verfasserin aut Cottle, John verfasserin aut Salado Paz, Natalia verfasserin aut Glodny, Johannes verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 776 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:776 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 776 |
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10.1016/j.tecto.2019.228276 doi (DE-627)ELV003659666 (ELSEVIER)S0040-1951(19)30391-9 DE-627 ger DE-627 rda eng 550 DE-600 38.36 bkl 38.58 bkl Payrola, Patricio verfasserin (orcid)0000-0001-8697-5914 aut Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera del Papa, Cecilia verfasserin aut Aramayo, Alejandro verfasserin aut Pingel, Heiko verfasserin aut Hongn, Fernando verfasserin aut Sobel, Edward R. verfasserin aut Zeilinger, Gerold verfasserin aut Strecker, Manfred R. verfasserin aut Zapata, Sebastian verfasserin aut Cottle, John verfasserin aut Salado Paz, Natalia verfasserin aut Glodny, Johannes verfasserin aut Enthalten in Tectonophysics Amsterdam [u.a.] : Elsevier, 1964 776 Online-Ressource (DE-627)320505952 (DE-600)2012830-7 (DE-576)098474197 1879-3266 nnns volume:776 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.36 Tektonik 38.58 Geomechanik AR 776 |
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Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera |
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Payrola, Patricio @@aut@@ del Papa, Cecilia @@aut@@ Aramayo, Alejandro @@aut@@ Pingel, Heiko @@aut@@ Hongn, Fernando @@aut@@ Sobel, Edward R. @@aut@@ Zeilinger, Gerold @@aut@@ Strecker, Manfred R. @@aut@@ Zapata, Sebastian @@aut@@ Cottle, John @@aut@@ Salado Paz, Natalia @@aut@@ Glodny, Johannes @@aut@@ |
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Payrola, Patricio |
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Payrola, Patricio ddc 550 bkl 38.36 bkl 38.58 misc Central Andes misc NW Argentina misc Unconformities misc Orogenic Wedge misc U-Pb zircon geochronology misc Apatite U-Th/He thermochronology misc Eocene-to-Miocene multiple fault reactivations misc Basement-involved faults and non-systematic propagation of deformation misc Structural geology misc U-Pb geochronology misc Salta (Payogastilla) foreland misc Eastern Cordillera Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina |
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550 DE-600 38.36 bkl 38.58 bkl Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina Central Andes NW Argentina Unconformities Orogenic Wedge U-Pb zircon geochronology Apatite U-Th/He thermochronology Eocene-to-Miocene multiple fault reactivations Basement-involved faults and non-systematic propagation of deformation Structural geology U-Pb geochronology Salta (Payogastilla) foreland Eastern Cordillera |
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ddc 550 bkl 38.36 bkl 38.58 misc Central Andes misc NW Argentina misc Unconformities misc Orogenic Wedge misc U-Pb zircon geochronology misc Apatite U-Th/He thermochronology misc Eocene-to-Miocene multiple fault reactivations misc Basement-involved faults and non-systematic propagation of deformation misc Structural geology misc U-Pb geochronology misc Salta (Payogastilla) foreland misc Eastern Cordillera |
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Payrola, Patricio del Papa, Cecilia Aramayo, Alejandro Pingel, Heiko Hongn, Fernando Sobel, Edward R. Zeilinger, Gerold Strecker, Manfred R. Zapata, Sebastian Cottle, John Salado Paz, Natalia Glodny, Johannes |
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episodic out-of-sequence deformation promoted by cenozoic fault reactivation in nw argentina |
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Episodic out-of-sequence deformation promoted by Cenozoic fault reactivation in NW Argentina |
| abstract |
The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. |
| abstractGer |
The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. |
| abstract_unstemmed |
The Central Andes are the product of contractional deformation related to subduction of the Nazca plate beneath the South American continent. In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model. |
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In this geodynamic setting, thrust belt propagation in the Central Andean retroarc in NW Argentina and southern Bolivia has been linked with the critical wedge model implying progressive eastward migration of the deformation front during the Cenozoic. However, Eocene unconformities and growth strata within the orogenic hinterland of the Eastern Cordillera and Puna Plateau suggest selective reactivation of pre-Andean and Andean faults revealing a pattern of diachronous and spatially disparate range uplifts. The Calchaquí Valley in NW Argentina is characterized by basin-and-range morphology, which is intimately linked with the heterogeneous Neoproterozoic basement, Cretaceous rift structures, and the Cenozoic foreland. In this study, we analyze this complex deformation by reconstructing Cenozoic fault reactivation and sedimentation patterns in the Eastern Cordillera. Detailed structural mapping along the eastern Calchaquí border (Tonco area) reveals five Cenozoic unconformities in the former foreland deposits related to multiple episodes of fault reactivation during the Eocene-to-Pleistocene. A refined chronostratigraphy (U-Pb zircon), new AHe thermochronological data (apatite U-Th-Sm/He), and existing evidence for deformation indicate episodic out-of-sequence deformation and increased Eo-Oligocene (Puna Plateau) to Miocene (Eastern Cordillera) fault displacement apparently controlled by pre-Cenozoic heterogeneities. The coeval eastward propagation of deformation and continuing deformation in the west generally challenge the applicability of the critical wedge model.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Central Andes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">NW Argentina</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Unconformities</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Orogenic Wedge</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">U-Pb zircon geochronology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Apatite U-Th/He thermochronology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eocene-to-Miocene multiple fault reactivations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Basement-involved faults and non-systematic 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