Distributed deformation around the eastern tip of the Kunlun fault

Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relativel...
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Autor*in:	Kirby, Eric [verfasserIn] Harkins, Nathan

Format:	Artikel
Sprache:	Englisch

Erschienen:	2013

Schlagwörter:	Tibetan plateau Active tectonics Tectonic geomorphology Strike-slip faults

Anmerkung:	© Springer-Verlag Berlin Heidelberg 2013

Übergeordnetes Werk:	Enthalten in: International journal of earth sciences - Springer Berlin Heidelberg, 1999, 102(2013), 7 vom: 07. März, Seite 1759-1772
Übergeordnetes Werk:	volume:102 ; year:2013 ; number:7 ; day:07 ; month:03 ; pages:1759-1772

Links:	Volltext

DOI / URN:	10.1007/s00531-013-0872-x

Katalog-ID:	OLC2070426173

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520			\|a Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern ~200 km of the Kunlun fault, from >10 mm/year to <1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments.
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spelling	10.1007/s00531-013-0872-x doi (DE-627)OLC2070426173 (DE-He213)s00531-013-0872-x-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Kirby, Eric verfasserin aut Distributed deformation around the eastern tip of the Kunlun fault 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2013 Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern ~200 km of the Kunlun fault, from >10 mm/year to <1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments. Tibetan plateau Active tectonics Tectonic geomorphology Strike-slip faults Harkins, Nathan aut Enthalten in International journal of earth sciences Springer Berlin Heidelberg, 1999 102(2013), 7 vom: 07. März, Seite 1759-1772 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:102 year:2013 number:7 day:07 month:03 pages:1759-1772 https://doi.org/10.1007/s00531-013-0872-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_24 GBV_ILN_30 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_608 GBV_ILN_788 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4320 AR 102 2013 7 07 03 1759-1772
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language	English
source	Enthalten in International journal of earth sciences 102(2013), 7 vom: 07. März, Seite 1759-1772 volume:102 year:2013 number:7 day:07 month:03 pages:1759-1772
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author	Kirby, Eric
spellingShingle	Kirby, Eric ddc 550 ssgn 13 misc Tibetan plateau misc Active tectonics misc Tectonic geomorphology misc Strike-slip faults Distributed deformation around the eastern tip of the Kunlun fault
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topic_title	550 VZ 13 ssgn Distributed deformation around the eastern tip of the Kunlun fault Tibetan plateau Active tectonics Tectonic geomorphology Strike-slip faults
topic	ddc 550 ssgn 13 misc Tibetan plateau misc Active tectonics misc Tectonic geomorphology misc Strike-slip faults
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title	Distributed deformation around the eastern tip of the Kunlun fault
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title_full	Distributed deformation around the eastern tip of the Kunlun fault
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title_sort	distributed deformation around the eastern tip of the kunlun fault
title_auth	Distributed deformation around the eastern tip of the Kunlun fault
abstract	Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern ~200 km of the Kunlun fault, from >10 mm/year to <1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments. © Springer-Verlag Berlin Heidelberg 2013
abstractGer	Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern ~200 km of the Kunlun fault, from >10 mm/year to <1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments. © Springer-Verlag Berlin Heidelberg 2013
abstract_unstemmed	Abstract Whether active strain within the Indo-Asian collision zone is primarily localized along major strike-slip fault systems or is distributed throughout the intervening crust between faults remains uncertain. Despite refined estimates of slip rates along many of the major fault zones, relatively little is known about how displacement along these structures is accommodated at fault terminations. Here, we show that a systematic decrease in left-lateral slip rates along the eastern ~200 km of the Kunlun fault, from >10 mm/year to <1 mm/year, is coincident with high topography in the Anyemaqen Shan and with a broad zone of distributed shear and clockwise vorticity within the Tibetan Plateau. Geomorphic analysis of river longitudinal profiles, coupled with inventories of cosmogenic radionuclides in fluvial sediment, reveal correlated variations in fluvial relief and erosion rate across the Anyemaqen Shan that reflect ongoing differential rock uplift across the range. Our results imply that the termination of the Kunlun fault system is accommodated by a combination of distributed crustal thickening and by clockwise rotation of the eastern fault segments. © Springer-Verlag Berlin Heidelberg 2013
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title_short	Distributed deformation around the eastern tip of the Kunlun fault
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