Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru
The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermome...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hughes, Cameron A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020transfer abstract |
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| Übergeordnetes Werk: |
Enthalten in: Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community - Borri, Maria ELSEVIER, 2020, international journal of geotectonics and the geology and physics of the interior of the earth, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:794 ; year:2020 ; day:5 ; month:11 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1016/j.tecto.2020.228610 |
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ELV051843412 |
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| 245 | 1 | 0 | |a Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru |
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| 520 | |a The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. | ||
| 520 | |a The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. | ||
| 700 | 1 | |a Jessup, Micah J. |4 oth | |
| 700 | 1 | |a Shaw, Colin A. |4 oth | |
| 700 | 1 | |a Newell, Dennis L. |4 oth | |
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10.1016/j.tecto.2020.228610 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001183.pica (DE-627)ELV051843412 (ELSEVIER)S0040-1951(20)30293-6 DE-627 ger DE-627 rakwb eng 610 VZ 44.63 bkl Hughes, Cameron A. verfasserin aut Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. Jessup, Micah J. oth Shaw, Colin A. oth Newell, Dennis L. oth Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:794 year:2020 day:5 month:11 pages:0 https://doi.org/10.1016/j.tecto.2020.228610 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 794 2020 5 1105 0 |
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10.1016/j.tecto.2020.228610 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001183.pica (DE-627)ELV051843412 (ELSEVIER)S0040-1951(20)30293-6 DE-627 ger DE-627 rakwb eng 610 VZ 44.63 bkl Hughes, Cameron A. verfasserin aut Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. Jessup, Micah J. oth Shaw, Colin A. oth Newell, Dennis L. oth Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:794 year:2020 day:5 month:11 pages:0 https://doi.org/10.1016/j.tecto.2020.228610 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 794 2020 5 1105 0 |
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10.1016/j.tecto.2020.228610 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001183.pica (DE-627)ELV051843412 (ELSEVIER)S0040-1951(20)30293-6 DE-627 ger DE-627 rakwb eng 610 VZ 44.63 bkl Hughes, Cameron A. verfasserin aut Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. Jessup, Micah J. oth Shaw, Colin A. oth Newell, Dennis L. oth Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:794 year:2020 day:5 month:11 pages:0 https://doi.org/10.1016/j.tecto.2020.228610 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 794 2020 5 1105 0 |
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10.1016/j.tecto.2020.228610 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001183.pica (DE-627)ELV051843412 (ELSEVIER)S0040-1951(20)30293-6 DE-627 ger DE-627 rakwb eng 610 VZ 44.63 bkl Hughes, Cameron A. verfasserin aut Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. Jessup, Micah J. oth Shaw, Colin A. oth Newell, Dennis L. oth Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:794 year:2020 day:5 month:11 pages:0 https://doi.org/10.1016/j.tecto.2020.228610 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 794 2020 5 1105 0 |
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10.1016/j.tecto.2020.228610 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001183.pica (DE-627)ELV051843412 (ELSEVIER)S0040-1951(20)30293-6 DE-627 ger DE-627 rakwb eng 610 VZ 44.63 bkl Hughes, Cameron A. verfasserin aut Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. Jessup, Micah J. oth Shaw, Colin A. oth Newell, Dennis L. oth Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:794 year:2020 day:5 month:11 pages:0 https://doi.org/10.1016/j.tecto.2020.228610 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 794 2020 5 1105 0 |
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evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the cordillera blanca, peru |
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Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru |
| abstract |
The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. |
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The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. |
| abstract_unstemmed |
The Cordillera Blanca shear zone (CBSZ) occupies the footwall of the Cordillera Blanca detachment fault, an active low-moderate angle detachment fault extending for ~200 km along the western margin of the Cordillera Blanca in central Peru. Recrystallized quartz paleopiezometry, two-feldspar thermometry on asymmetric strain-induced myrmekite, and structural analysis from the CBSZ provide evidence for shear zone evolution within a transient elevated geotherm during syn-convergent extension. Shear zone width varies by a factor of six along strike, with widths of up to ~400 m within the central segment of the shear zone. Microstructurally-derived strain rates, calculated from quartz paleopiezometry and two-feldspar thermometry results, are on the order of 10−14 to 10−12 s−1 and are broadly consistent with macrostructurally-derived strain rates of 10−14 to 10−13 s−1 calculated from shear zone thickness and previously determined exhumation rates. Within the context of existing thermochronological data, constraints on batholith emplacement, and previously determined offset along the Cordillera Blanca detachment, our data suggest that ductile deformation in the CBSZ occurred within a transient elevated geothermal gradient of at least ~50 °C/km and potentially as high as ~100 °C/km, which deviated from a ~30 °C/km gradient for an unspecified duration of time. We discuss the evolution of the Cordillera Blanca, where observed deformation fabrics are related to strain localization along an exhuming fault as well as thermal weakening from the interplay between faulting and magmatism. |
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Evidence for strain rate variation and an elevated transient geothermal gradient during shear zone evolution in the Cordillera Blanca, Peru |
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