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祁连山-河西走廊现今垂直形变特征与区域应力场
引用本文:王双绪,江在森,张四新.祁连山-河西走廊现今垂直形变特征与区域应力场[J].大地测量与地球动力学,1997(1).
作者姓名:王双绪  江在森  张四新
作者单位:国家地震局第二地形变监测中心
摘    要:利用多期地形变监测资料,研究了祁连山-河西走廊地区七十年代初至今的大地垂直形变演化与构造活动特征。认为,构造形变特征与青藏高原挤压作用为主导的区域应力场消长变化有关,目前祁连山相对走廊盆地下沉,具有较弱的逆继承性运动特征,表明在1988~1990年青藏块体应变能大释放之后区域应力场处于松驰、调整阶段

关 键 词:垂直形变  应力场  祁连山-河西走廊

CHARACTERISTICS OF THE RECENT VERTICAL DEFORMATION AND THE REGIONAL STRESS FIELD IN QILIAN MOUTIAN-HEXI CORRIDOR
Wang Shuangxu,Jiang Zaisen and Zhang Sixin.CHARACTERISTICS OF THE RECENT VERTICAL DEFORMATION AND THE REGIONAL STRESS FIELD IN QILIAN MOUTIAN-HEXI CORRIDOR[J].Journal of Geodesy and Geodynamics,1997(1).
Authors:Wang Shuangxu  Jiang Zaisen and Zhang Sixin
Abstract:Based on the monitoring data of crustal deformation, the characteristics of the vertical deformation and tectonic activity in Qilian mountian-Hexi corridor area since the 1970s are studied. It is concluded that the Qilian mountian sinks relatively to Hexi corridor basin and makes a feature of weak inherited inverse motion at present, which shows that the stress field in the area is in a period of relaxation and adjustment after the strain energy in Qing-Zang block released from 1988 to 1990.
Keywords:vertical deformation  stress field  Qilian mountian-Hexi corridor
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