Geometry and kinematics of Cenozoic right-lateral strike-slip thrust structural belt in the north margin of the Qaidam Basin(柴达木盆地北缘新生代右行走滑冲断构造带的几何学和运动学)

Geometry and kinematics of Cenozoic right-lateral strike-slip thrust structural belt in the north margin of the Qaidam Basin(柴达木盆地北缘新生代右行走滑冲断构造带的几何学和运动学)

通过露头地质调查、地震剖面解释和地层残余厚度图的分析，发现柴达木盆地北缘新生代以右行走滑冲断构造变形为主.走滑冲断构造带内的断层在平面上呈分支复合，剖面上表现为花状构造，走滑逆冲断层上、下盘地层呈不协调产出.右行走滑冲断构造带形成的应力来源于阿尔金断裂左行走滑的拖拽力作用以及北东-南西和北西-南东向的简单剪切应力作用....

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Bibliographic Details
Main Authors: WANGBu-qing(王步清), XIAOAn-cheng(肖安成), CHENGXiao-gan(程晓敢), HEGuang-yu(何光玉), CHENHan-lin(陈汉林), YANGShu-fcng(杨树锋)
Format: Article
Language:zho
Published: Zhejiang University Press 2005-05-01
Series:Zhejiang Daxue xuebao. Lixue ban
Subjects:
柴达木盆地
走滑冲断构造带
几何学
运动学
Online Access:https://doi.org/zjup/1008-9497.2005.32.2.225-230

Internet

https://doi.org/zjup/1008-9497.2005.32.2.225-230

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