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| 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 |
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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.
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Received: 06 September 2007
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2008, Vol. 17 
