THE TRIASSIC LEFT-LATERAL DUCTILE SHEAR ZONE OF TAN-LU FAULT ZONE AND ITS DEFORMATION IN NORTHERN LIAONING PROVINCE
LI Dong-tao1, HU Jin-wei1, LI Jing-hong1, SUN Peng-hui1, WANG Xiao-ou1, LIU Zhong-yuan2
1. Liaoning Institute of Geologic and Mineral Resources Survey, Shenyang 110032, China; 2. Liaoning Bureau of Geology and Mineral Resources Exploration, Shenyang 110032, China
Abstract：The section of Tan-Lu fault zone in northern Liaoning Province, as a part of Yilan-Yitong fault zone, is actually the regional northward extension of the Tan-Lu fault zone. The NE-trending Triassic left-lateral ductile shear zone is discovered during the regional geological survey in 1:50000 scale. The ductile shear zone controls the distribution of a series of Triassic intrusive rocks and reforms the extension of Paleozoic geologic bodies.
李东涛, 胡晋伟, 李景弘, 孙鹏慧, 王晓鸥, 刘忠元. 郯庐断裂带在辽北地区三叠纪左行韧性剪切带的发现及变形特征[J]. 地质与资源, 2008, 17(4): 254-258.
LI Dong-tao, HU Jin-wei, LI Jing-hong, SUN Peng-hui, WANG Xiao-ou, LIU Zhong-yuan. THE TRIASSIC LEFT-LATERAL DUCTILE SHEAR ZONE OF TAN-LU FAULT ZONE AND ITS DEFORMATION IN NORTHERN LIAONING PROVINCE. GEOLOGY AND RESOURCES, 2008, 17(4): 254-258.
2008, Vol. 17 
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