Late Pleistocene‐Holocene Slip Rate Along the Hasi Shan Restraining Bend of the Haiyuan Fault: Implication for Faulting Dynamics of a Complex Fault System - Archive ouverte HAL
Journal Articles Tectonics Year : 2019

Late Pleistocene‐Holocene Slip Rate Along the Hasi Shan Restraining Bend of the Haiyuan Fault: Implication for Faulting Dynamics of a Complex Fault System

Rémi Matrau
  • Function : Author
Yann Klinger
Jerome van Der Woerd
Institut de physique du globe de Strasbourg
CV
Jing Liu‐zeng
  • Function : Author
Zheng Li
Xiwei Xu
Rongzhang Zheng
  • Function : Author

Abstract

Slip rate along the Hasi Shan section of the Haiyuan fault is determined from numerous offsets and cosmogenic exposure dates over a period of 50000 years.

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Tectonics
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https://hal.science/hal-03027728

Submitted on : Friday, November 27, 2020-12:26:32 PM

Last modification on : Monday, December 2, 2024-2:48:11 PM

Long-term archiving on : Sunday, February 28, 2021-7:18:23 PM

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hal-03027728 , version 1 (27-11-2020)

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Rémi Matrau, Yann Klinger, Jerome van Der Woerd, Jing Liu‐zeng, Zheng Li, et al.. Late Pleistocene‐Holocene Slip Rate Along the Hasi Shan Restraining Bend of the Haiyuan Fault: Implication for Faulting Dynamics of a Complex Fault System. Tectonics, 2019, 38 (12), pp.4127-4154. ⟨10.1029/2019TC005488⟩. ⟨hal-03027728⟩

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