Quaternary activity along the Tan-Lu fault zone in the Bohai Bay, East China: Evidence from seismic profiles
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- 作者：Guang Zhu ; zhuguang59@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Wei Hu hw0958@163.com" class="auth_mail" title="E-mail the corresponding author ; Lihong Song song.l.h@163.com" class="auth_mail" title="E-mail the corresponding author ; Bei Liu liubei4820208@163.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Tan-Lu fault zone ; Latest seismic activity ; Kinematics ; Earthquake ; Bohai Bay
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：15 December 2015
- 年：2015
- 卷：114
- 期：part_P1
- 页码：5-17
- 全文大小：15284 K
文摘
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The Quaternary Tan-Lu fault zone in the Bohai Bay consists of two main faults dipping steeply to the west.
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The Tan-Lu fault zone was dominated by reverse dextral slip during the Holocene.
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The Tan-Lu fault zone in the southern and central sections of the Bohai Bay was last active during the Holocene.
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The ENE–WSW compression led to the Holocene faulting associated with many recent earthquakes in the Bohai Bay.