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点位错引起的单层密度变化
引用本文:申重阳,甘家思,朱思林,徐菊生.点位错引起的单层密度变化[J].大地测量与地球动力学,1997(1).
作者姓名:申重阳  甘家思  朱思林  徐菊生
作者单位:国家地震局地震研究所
摘    要:采用求解地壳单层密度变化的一般公式,导出其平面近似公式并给出了相应的数值计算方法。在此基础上,将点位错引起的地表形变和重力变化同时解析延拓至Bjerhammar球面上,得到了点位错引起的地壳单层密度变化的图像。分析表明:①单层密度变化图像与地表形变、重力变化图像相似;②地表形变对单层密度变化的影响比地表重力变化要大;③若点位错引起地表重力变化为10-6~10-7m/s2量级、高程变化为0.1~1m量级,则单层密度变化可达103~104kg/m2量级;④单层密度变化在隆升区为正,沉降区为负

关 键 词:位错  密度  重力  垂直形变

SINGLE-LAYER DENSITY CHANGES CAUSED BY POINT DISLOCATIONS
Shen Changyang,Gan Jiasi,Zhu Silin and Xu Jusheng.SINGLE-LAYER DENSITY CHANGES CAUSED BY POINT DISLOCATIONS[J].Journal of Geodesy and Geodynamics,1997(1).
Authors:Shen Changyang  Gan Jiasi  Zhu Silin and Xu Jusheng
Abstract:By use of the common formula for solving the time variations of the crustal density, the approximative plane formula is derived and its numerical calculation method is given. Accordingly, the surface deformation and gravity changes caused by point dislocations are analyzed and continuated to the Bjerhammar shpere,then the graph of single-layer density changes raised by point dislocations is calculated.The result shows:(1)The graph of single-layer density changes is similar to the surface deformation and gravity changes,(2)The effect of surface deformations on the single-layer density changes is larger than the surface gravity changes,(3)If the surface gravity changes caused by point dislocation are the level of 10 -6 or 10 -7 m/s 2 and the surface topographic changes are the level of 0.1 or 1.0m,the single-layer density changes will reach the level of 10 3 or 10 4kg/m 2,(4)the single-layer density changes are positive on the uplife area and negative on the subsidence area.
Keywords:dislocation  density  gravity  vertical deformation
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