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Stable rate of slip along the Karakax section of the Altyn Tagh Fault from observation of inter-glacial and post-glacial offset morphology and surface dating

Lookup NU author(s): Dr Anne-Sophie Meriaux

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This is the authors' accepted manuscript of an article that has been published in its final definitive form by American Geophysical Union; Wiley-Blackwell Publishing, Inc., 2020.

For re-use rights please refer to the publisher's terms and conditions.


Abstract

Key Points: Offset alluvial fans in Karakax Valley record sinistral displacement history along Altyn Tagh Fault Terrace ages determined by OSL and CRN dating methods yield fault slip-rate of 2.6 mm/a over 115 ka Seismic clustering or variable erosion rate linked to climate may explain observed fault scarp degradation variations


Publication metadata

Author(s): Peltzer G, Brown N, Meriaux AS, van der Woerd J, Rhodes E, Finkel R, Ryerson F, Hollingsworth J

Publication type: Article

Publication status: Published

Journal: Journal of Geophysical Research - Solid Earth

Year: 2020

Volume: 125

Issue: 5

Print publication date: 06/05/2020

Online publication date: 06/04/2020

Acceptance date: 04/03/2020

Date deposited: 27/05/2020

ISSN (print): 2169-9313

ISSN (electronic): 2169-9356

Publisher: American Geophysical Union; Wiley-Blackwell Publishing, Inc.

URL: https://doi.org/10.1029/2019JB018893

DOI: 10.1029/2019JB018893


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