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祁连山中段构造应力场特征研究
引用本文:张向红,杨斌,周俊喜,刘洪春. 祁连山中段构造应力场特征研究[J]. 高原地震, 2005, 17(4): 10-17
作者姓名:张向红  杨斌  周俊喜  刘洪春
作者单位:甘肃省地震局,甘肃,兰州,730000;甘肃省地震局,甘肃,兰州,730000;甘肃省地震局,甘肃,兰州,730000;甘肃省地震局,甘肃,兰州,730000
摘    要:试图通过水系、构造和现代资料的反演来对祁连山中段中晚更新世以来及现代构造应力场特征的研究,来表明构造应力场具有明显的分区性,且主压应力方向由北向南发生渐变,角度逐渐增大。

关 键 词:祁连山中段  构造应力场  主压应力
文章编号:1005-586X(2005)04-0010-08
收稿时间:2005-08-12
修稿时间:2005-11-02

STUDY ON TECTONIC STRESS FIELD CHARACTERISTICS IN MIDDLE SECTION OF QILIAN MOUNTAIN
ZHANG Xiang-hong,YANG Bin,ZHOU Jun-xi,LIU Hong-chun. STUDY ON TECTONIC STRESS FIELD CHARACTERISTICS IN MIDDLE SECTION OF QILIAN MOUNTAIN[J]. Plateau Earthquake Research, 2005, 17(4): 10-17
Authors:ZHANG Xiang-hong  YANG Bin  ZHOU Jun-xi  LIU Hong-chun
Affiliation:Earthquake Adminstration of Gansu Province, Lanzhou 730000, China
Abstract:In an effort to study the characteristics of tectonic stress fded of middle section of Qilian Mountain since middle and later Pleistocene to that of present, reversion analysis on drainage system, tectonic and present evidences is carried out. The results show that there is clear tectonic stress field division in the region and the orientation of the principal compressive stress gradually increases from north part to south part of the region.
Keywords:Middle section of Qilian Mountain   Tectonic stress field   Principal compressive stress
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