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中国科学院大学学报 ›› 2013, Vol. 30 ›› Issue (1): 74-82.DOI: 10.7523/j.issn.1002-1175.2013.01.012

• 地球科学 • 上一篇    下一篇

GPS约束下川滇地区主要断裂现今活动速率的估算方法

郭晓虎1,2, 魏东平1,2, 张克亮3   

  1. 1. 中国科学院计算地球动力学重点实验室, 北京 100049;
    2. 中国科学院研究生院地球科学学院, 北京 100049;
    3. 中国地震局地质研究所地震动力学国家重点实验室, 北京 100029
  • 收稿日期:2012-01-19 修回日期:2012-03-28 发布日期:2013-01-15
  • 通讯作者: 魏东平
  • 基金资助:

    国家自然科学基金(41174084)资助

GPS-constrained estimate method of present-day slip rate along major faults of Sichuan-Yunnan region in China

GUO Xiao-Hu1,2, WEI Dong-Ping1,2, ZHANG Ke-Liang3   

  1. 1. Key Laboratory of Computational Geodynamics, Graduate University, Chinese Academy of Sciences, Beijing 100049, China;
    2. College of Earth Science, Graduate University, Chinese Academy of Sciences, Beijing 100049, China;
    3. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2012-01-19 Revised:2012-03-28 Published:2013-01-15

摘要:

以川滇地区的GPS水平速度场为约束,建立由24个块体组成的线性弹性块体模型,剔除块体内部变形等对GPS测站速度的影响,反演得到各块体的长期运动速度及各主要边界断裂的现今活动速率.结果显示,在考虑块体内部弹性形变时,拟合速度残差中误差由1.46mm/a减小至1.15mm/a.因此,在用块体模型分析复杂构造地区的运动特征时,还需顾及块体内部形变的影响.

关键词: 川滇地区, GPS, 断裂活动速率, 块体模型, 欧拉矢量

Abstract:

In order to obtain the long-term motions of blocks and contemporary slip rates along major bounding faults in Sichuan-Yunnan region,we built a GPS-constrained linear elastic block model with 24 blocks and eliminated the effect of internal deformation of each block. After the elimination of internal deformation effect,the results show that the RMSE of residual velocities decreased from 1.46 mm/a to 1.15 mm/a. Therefore, one should consider the elastic internal deformation effect when analyzing the motion characteristics of tectonically complicated region using block model.

Key words: Sichuan-Yunnan region, GPS, slip rate, block model, Euler vector

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