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SOME VIEWPOINTS ABOUT THE YALUJIANG MAJOR FAULT ZONE IN LYUJIANGCUN AREA, LIAONING PROVINCE |
PAN Ming-chen |
Liaoning Institute of Geological Exploration, Dalian 116100, Liaoning Province, China |
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Abstract The Yalujiang fault zone is a branch the Tan-Lu giant fault zone, which crosses eastern China. Its dynamic mechanism is the collision between the Pacific plate and Eurasian plate during Yanshanian period. The shearing movement forms a series of NE-trending sinistral crustal fractures, in depth about 4 km, with maximal left displacement more than 20 km. The geological structural characteristics on both sides of the major fault are comparable.
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Received: 23 December 2015
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