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The Linking between Nappe Structures in Northwestern Yunkai Block and Indosinian Orogeny
详细信息   
摘要
Along Luoding-Guangning fault of northwest edge of Yunkaidashan block,several NE shallow thrusting overthrust structure trending to the SE are found.Those thrust tectonics and strike-slip fault zones constitute flower structure,with continental crust remelting granite emplacement,is part of Indosinian orogenic system of northwest margin of Yunkaidashan Block.

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