Mesozoic reactivated transpressional structures and multi-stage tectonic deformation along the Hong-Che fault zone in the northwestern Junggar Basin, NW China
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- 作者：Yangli Yu ; Xin Wang ; zjuwx@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; wx@zju.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Gang Rao ; Renfu Wang1
- 关键词：Seismic profiling ; Strike-slip fault ; Hong-Che fault zone ; NW Junggar
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：4 June 2016
- 年：2016
- 卷：679
- 期：Complete
- 页码：156-168
- 全文大小：4781 K
文摘
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We demonstrate the Hong-Che fault zone in NW Junggar basin is a buried paleo-strike-slip fault.
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The dextral strike-slip faulting prevailed in the Junggar Basin during the Middle Triassic to Late Jurassic.
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The Early Permian-Late Jurassic multi-phase deformation along the NW margin of Junggar basin is demonstrated.