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《Geology of Chemical Minerals》 2003-01
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The Structure Style of Yanshan and the Western Liaoning

Lin Xiaohui Qin Zhengyong (Tianjin Institute of Geology and Mineral Resources)  
The structure style of Yanshan and the western Liaoning consists of a synclinorium and an antiform. The synclinorium consists of E-W three longitudinal anticlines and two longitudinal synclines, the E-W longitudinal axis faults, S-N cross faults and NE, NW X-shaped faults. Shangyi-Kuancheng-Pepeifault is the longitudinal axis fault. The mid-low Jurassic series are its fissure fillings. Qinhuangdao antiform is as a result of NE-shearred western Liaoning along Qinhuangdao-Iinyan axis fault. The synclinorium has been reconstruted into the second Ramsay' s fold style. The NNE has overlaped the NE of X-shaped faults in Yanshan and the longitudinal faults in the western Liaoning. The geomdynamic mechanism of synclinoriuni is suitable to the buckle folding.
【CateGory Index】: P542
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