Quaternary faulting of the Jiangsu part of the Tan-Lu Fault Zone, East China: Evidence from field investigations and OSL dating
详细信息 查看全文
- 作者：Bei Liu liubei4820208@163.com" class="auth_mail" title="E-mail the corresponding author ; Guang Zhu ; zhuguang59@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Mingjiang Zhai zhaimingjian199110@163.com" class="auth_mail" title="E-mail the corresponding author ; Chengchuan Gu gucheng102@126.com" class="auth_mail" title="E-mail the corresponding author ; Shuo Liu 1073049632@qq.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Jiangsu part of the Tan-Lu Fault Zone ; Kinematics ; Stress field ; OSL dating ; Timing of fault activity
- 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：89-102
- 全文大小：8301 K
文摘
- •
The Jiangsu part of the Tan-Lu Fault Zone shows widespread activity during Quaternary.
- •
The main Quaternary faults show evidence of thrusting with a minor dextral component.
- •
The ENE–WSW compression was responsible for the Quaternary faulting.
- •
The most recent period of activity was the late Pleistocene, which is consistent with the absence of M ⩾ 4.0 earthquakes.
- •
The main active faults originated from reactivation of the Cretaceous graben-boundary faults.