地震地质 ›› 1995, Vol. 17 ›› Issue (1): 25-31.

• 科研简报 • 上一篇    下一篇

倾斜断层深部不均匀滑动的反演计算

刘洁1, 宋惠珍1, 巫映祥2, 刘贵梅2   

  1. 1. 国家地震局地质研究所, 北京, 100029;
    2. 国家地震局地壳应力研究所, 北京, 100039
  • 收稿日期:1993-07-31 修回日期:1994-07-31 出版日期:1995-03-08 发布日期:2009-11-25
  • 基金资助:
    地震科学联合基金资助(89054)

INVERSION OF DEEP SLIP OF INCLINED-FAULT FROM GEODETIC DATA

Liu Jie1, Song Huizhen1, Wu Yingxiang2, Liu Guimei2   

  1. 1. Institute of Geology, State Seismological Bureau, Beijing 100029;
    2. Institute of Crustal Dynamics, State Seismological Bureau, Beijing 100039
  • Received:1993-07-31 Revised:1994-07-31 Online:1995-03-08 Published:2009-11-25

摘要: 根据倾斜断层走滑、倾滑及拉张运动产生的地表位移计算公式,利用Harris和Segall的反演方法,建立了倾斜断层具多个滑动分量的反演模型,编制了相应的计算机程序,实现了利用大地测量资料反演计算不同产状断层深部不同运动方向的滑动速率或滑动量。并以北京地区两条主要活动断层为例进行了计算,获得结果与北京地区区域应力场及断层应力场具有较好的一致性。

关键词: 大地形变测量, 反演模型, 断层滑动, 断层位移速率

Abstract: In this paper,according to the calculating formula for the surface displacements related to an inclined,shear and tensile fault,an inverse model of inclined fault has been established,by use of Segall and Harris'method.A FORTRAN program has been given also,by which the deep slip rate and deep slip value of different attitude fault in different motion components can be inversed.So,the slip rate of two faults in Beijng area have been calculated.The activity of main active faults in Beijing area are well coincident with the regional stress field and fault stress field.

Key words: Geodetic deformation measurement, Inversion model, Fault slip, ault displacement rate