Tectonic-geomorphology of the Litang fault system, SE Tibetan Plateau, and implication for regional seismic hazard
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- 作者：Marie-Luce Chevaliera ; mlchevalier@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Philippe Hervé ; Leloupb ; herve.leloup@univ-lyon1.fr" class="auth_mail" title="E-mail the corresponding author ; Anne Replumazc ; d ; anne.replumaz@ujf-grenoble.fr" class="auth_mail" title="E-mail the corresponding author ; Jiawei Pana ; jiawei-pan@foxmail.com" class="auth_mail" title="E-mail the corresponding author ; Dongliang Liua ; pillar131@163.com" class="auth_mail" title="E-mail the corresponding author ; Haibing Lia ; lihaibing06@163.com" class="auth_mail" title="E-mail the corresponding author ; Loraine Gourbetb ; e ; loraine.gourbet@ens-lyon.fr" class="auth_mail" title="E-mail the corresponding author ; Marianne Mé ; toisb ; marianne.metois@univ-lyon1.fr" class="auth_mail" title="E-mail the corresponding author
- 关键词：Litang fault system ; Eastern Tibet ; Slip-rate ; Tectonic-geomorphology ; Earthquake hazard ; Sichuan
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：6 July 2016
- 年：2016
- 卷：682
- 期：Complete
- 页码：278-292
- 全文大小：7436 K
文摘
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The Litang fault system (LTFS) is located in eastern Tibet
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We studied horizontally offset moraine crests at Cuopu and a vertically offset fan at Maoya along the LTFS
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The horizontal rate along the N Cuopu fault is ~ 2 mm/yr from 5.3 Ma to 29 ka
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The vertical rate at Maoya is constant at ~ 0.6 mm/yr since 5-7 Ma
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Its high segmentation, dominantly normal kinematics and low slip-rate reduce the risk of M > 7.5 earthquakes along the LTFS
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