• ISSN 2097-1893
  • CN 10-1855/P

全球定位系统数据所显示的华北平原现今形变

Y. G. Zhang W. J. Zheng Y. J. Wang D. L. Zhang Y. T. Tian M. Wang Z. Q. Zhang P. Z. Zhang 李莹甄 颜梓幸 赵爱华

引用本文: 李莹甄, 颜梓幸 译. 2020. 全球定位系统数据所显示的华北平原现今形变. 世界地震译丛. 51(1):75-85. doi:10.16738/j.cnki.issn.1003-3238.202001006

全球定位系统数据所显示的华北平原现今形变

doi: 10.16738/j.cnki.issn.1003-3238.202001006
基金项目: 

本译文由防灾科技学院教研教改项目(JY2017B01)、河北省教改项目(2017GJJG257)和防灾科技学院精品课项目(JPJS2018006)联合资助

  • 摘要: 华北平原是一个地震危险性很高的地区,但先前的全球定位系统测量显示,华北平原现今几乎没有地壳形变。利用中国东部三个块体的最新全球定位系统数据,发现华北平原的地震间形变发生在一个近东西向、宽约1 100km的左旋剪切带内。地震间的左旋剪切形变为6.0±1.3mm/a,其造成的现今形变最终被沿北—北东向断层、右旋走滑的地震破裂和块体的逆时针旋转所调节。我们认为刚性华南块体相对于刚性阿穆里安块体向东的快速运动,产生了一对左旋剪切力偶,扭曲了非刚性的华北平原,形成了现今的地壳形变。

     

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