首页 > 《地质学报：英文版》 > 2016年2期 > Revisiting Late Quaternary Slip-rate along the Maqu Segment of the Eastern Kunlun Fault, Northeast Tibet

Revisiting Late Quaternary Slip-rate along the Maqu Segment of the Eastern Kunlun Fault, Northeast Tibet

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摘要晚第四级沿着东方Kunlun差错的Maqu片断滑动率用高分辨率的遥感形象解释，地观察和微分全球放系统(GPS)的联合被估计偏移量河平台的大小，和14从偏移量起床人收集的蜗牛壳标明日期的C。结果证明沿着片断的离开滑倒率是3-5mm/a，并且垂直滑倒率是0.3-0.5mm/a。两水平、垂直在在∼100km的距离上一致的片断遗体上滑倒。当以前建议了，它意味着不滑动坡度沿着Maqu片断发生了，并且它可能因此作为一个独立seismogenic差错表现。在年轻梯田之中从多重关系判定抵消，我们推断典型地震在Maqu差错上与Ms7.0-7.5的大小生产的那co地震的表面破裂能产生一水平4.5-5m滑倒并且一垂直0.45-0.5m滑倒，与大约9的相应比率(Dh/Dv)。二个表面破裂事件肯定发生在过去的3300年，最近的可能在1485calBP和1730calBP之间。

DOI lder3mn943/1614765

作者 LI Jian;ZHANG Yueqiao;LI Hailong;XIONG Jinhong;LI Jianhua;WU Tairan

机构地区不详

出处《地质学报：英文版》 2016年2期

关键词东昆仑断裂滑动速率晚第四纪西藏东北部玛曲差分全球定位系统

分类 [天文地球][地质学]

出版日期 2016年02月12日（中国期刊网平台首次上网日期，不代表论文的发表时间）

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来源期刊

地质学报：英文版

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东昆仑断裂滑动速率晚第四纪西藏东北部玛曲差分全球定位系统

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