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乌鲁木齐地区近期地壳水平形变初步研究
引用本文:王晓强,张永岗,海力·阿不都热依木,李杰.乌鲁木齐地区近期地壳水平形变初步研究[J].内陆地震,2002,16(2):154-159.
作者姓名:王晓强  张永岗  海力·阿不都热依木  李杰
作者单位:新疆维吾尔自治区地震局,新疆乌鲁木齐,830011
摘    要:根据乌鲁木齐地区 2 0 0 0年、2 0 0 1年两期 GPS网资料及其它资料处理结果 ,讨论了乌鲁木齐现阶段应变场及监测区的断层水平运动情况。分析结果认为乌鲁木齐地区地壳整体主要受 NW方向的主压应力作用 ,乌鲁木齐测区大部分 GPS观测点以乌鲁木齐红山观测点为中心呈顺时针方向运动。

关 键 词:GPS监测网  水平形变  主压应力  剪应力  乌鲁木齐
文章编号:1001-8956(2002)02-0154-06
修稿时间:2001年12月10

PRELIMINARY STUDY ON RECENT HORIZONTALCRUSTAL DEFORMATION IN URUMQI AREA
WANG Xiao qiang,ZHANG Yong gang,Haili.Abudureyimu,LI Jie.PRELIMINARY STUDY ON RECENT HORIZONTALCRUSTAL DEFORMATION IN URUMQI AREA[J].Inland Earthquake,2002,16(2):154-159.
Authors:WANG Xiao qiang  ZHANG Yong gang  HailiAbudureyimu  LI Jie
Abstract:Based on two stages of GPS data during 2000 and 2001 in the Urumqi area and other data, recent strain field in Urumqi and the horizontal movements of the faults in monitoring region were analyzed. The result shows that the whole crust of the Urumqi area is mainly effected by principal compressive stress in NW direction, and the majority of GPS stations in Urumqi monitoring region are clockwise moving taking Hongshan observation station in Urumqi as center.
Keywords:GPS monitoring net  Horizontal deformation  Principal compressive stress  Shear stress  Urumqi
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