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

P542.2%P542.3; 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,发现柴迭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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Published in浙江大学学报（理学版） Vol. 32; no. 2; pp. 225 - 230
Main Authors 王步清, 肖安成, 程晓敢, 何光玉, 陈汉林, 杨树锋
Format Journal Article
LanguageChinese
Published 浙江大学,地球科学系,浙江,杭州,310027 2005
Subjects
运动学
柴达木盆地
几何学
走滑冲断构造带
Online AccessGet full text
ISSN1008-9497
DOI10.3321/j.issn:1008-9497.2005.02.027

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Abstract P542.2%P542.3; 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,发现柴迭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.
AbstractList P542.2%P542.3; 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,发现柴迭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.
Author 何光玉
肖安成
杨树锋
王步清
程晓敢
陈汉林
AuthorAffiliation 浙江大学,地球科学系,浙江,杭州,310027
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XIAO An-cheng
YANG Shu-feng
CHENG Xiao-gan
HE Guang-yu
WANG Bu-qing
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柴达木盆地
几何学
走滑冲断构造带
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Snippet P542.2%P542.3; 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,发现柴迭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,...
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Title 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
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