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地震 ›› 2006, Vol. 26 ›› Issue (2): 45-53.

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中国西部活动地块运动模型的建立及其运动学分析

刘卫华1,2, 魏东平1   

  1. 1.中国科学院研究生院计算地球动力学重点实验室, 北京 100049;
    2.中国科学院地质与地球物理研究所, 北京 100101
  • 收稿日期:2005-06-20 修回日期:2005-11-02 出版日期:2006-04-30 发布日期:2021-11-01
  • 作者简介:刘卫华(1978-), 男, 河北藁城人, 2003年在读硕士研究生, 现主要从事地球动力学等研究。
  • 基金资助:
    国家自然科学基金项目(40274035)

Study on current kinematic model of the active blocks in Western China by GPS survey data

LIU Wei-hua1,2, WEI Dong-ping1   

  1. 1. Laboratory of Computational Geodynamics, Graduate School of the Chinese Academy of Science, Beijing 100049;
    2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2005-06-20 Revised:2005-11-02 Online:2006-04-30 Published:2021-11-01

摘要: 中国西部的青藏和新疆地区现代构造变形活动非常强烈, 业已证实该区可以进一步划分为塔里木、 阿拉善、 天山、 柴达木和西藏5个活动地块。 利用GPS观测资料得到的中国大陆地壳水平运动的速度场, 借鉴全球板块运动模型的建模方法, 将其视为刚性的地块系统, 反演得到各地块相对欧亚板块运动的欧拉矢量, 进而求得各地块两两之间相对运动的欧拉矢量, 并计算出沿地块边界的相对运动速率。 结果显示, 与地块边界上的地震滑移矢量, 由地质学资料得到的滑移速率, 以及GPS数据本身均有较好的一致性, 从而也说明了将该地区划分为若干活动地块并视为刚性地块的合理性。

关键词: 中国西部, 活动地块, 板块运动, GPS, 欧拉矢量

Abstract: The neotectonic deformation is very strong along the Tibet and Xinjiang zone distributed in Western China. Nevertheless all the observed data of seismology and geology suggested that this area more possibly consists of several rigid blocks: the Tarim (TM), the Alashan (AS), the Qaidam (CD), the Tienshan (TS) and Tibet (TB). The kinematic model is mainly derived from the Global Positioning System (GPS) velocity data during the latest 10 years' observations, based on the method of the global plate model. The resulting Euler vectors predict that the movements of these microplates are consistent with the geophysical and geological observations of relative movements of the plates along their boundaries and that indicates it reasonable to regard these blocks as rigid ones.

Key words: Western China, Active block, Plate movement, GPS, Euler vectors

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