节点文献

三峡库首区现今构造应力场的形成体制分析

ANALYSIS OF THE FORMATION SYSTEM OF THE PRESENT TECTONIC STRESS FIELD IN THE HEAD AREA OF THE THREE GORGES RESERVOIR

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 李细光姚运生曾佐勋刘立林

【Author】 LI Xi-guang~1,YAO Yun-sheng~2,ZENG Zuo-xun~3,LIU Li-lin~3(1.Engineering Seismic Research Center,Seismological Bureau of Guangxi,Nanning,530022,Guangxi;2.Institute of Seismology,China Seismological Bureau,Wuhan,430071,Hubei; 3.School of Earth Sciences,China University of Geoscience,Wuhan 430074,Hubei)

【机构】 广西壮族地震局工程地震研究中心中国地震局地震研究所中国地质大学地球科学学院中国地质大学地球科学学院 南宁530022武汉430071武汉430074

【摘要】 本文从地质、地震、形变、地应力测量等方面对三峡库首区现今构造应力场进行了系统的分析和论证,并用数值模拟进行了验证,认为三峡库首区现今构造应力场属于纯剪切变形体制,即:在来自西部NE—SW方向主压应力挤压的基础上,同时叠加有因江汉—洞庭盆地拉张而引起的NWW—SEE向主张应力的作用,这两种力源近于直交,可以分别作为研究区现今构造应力场的主压应力(1σ)和主张应力(σ3)。

【Abstract】 The present tectonic stress field in the head area of the Three Gorges reservoir was systematically analyzed and verified in the geological,seismological,deformation and in situ stress contexts and checked by numerical modeling.The authors think that the present tectonic stress field in the study area belongs to a pure shear system,i.e.the superimposition of the NE-SW principal compressional stress from the west is superimposed by the WNW-ESE principal tensional stress resulting from extension of the Jianghan-Dongting basin.The axes of the two stresses intersect nearly perpendicularly to each other;so they can act as the principal compressive stress(σ1)and the principal tensional stress(σ3)of present tectonic stress field in the study area respectively.

【基金】 科技部“十.五”重点科技攻关项目“长江三峡水库诱发地震监测研究”(国科发财字[2002]484号)
  • 【文献出处】 地质力学学报 ,Journal of Geomechanics , 编辑部邮箱 ,2006年02期
  • 【分类号】P553
  • 【被引频次】12
  • 【下载频次】296
节点文献中: 

本文链接的文献网络图示:

本文的引文网络