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《World Nonferrous Metals》 2017-18
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Yunnan province Geological characteristics and genetic problems of copper polymetallic ore deposits in shangri-la county

LI Jun-fei;Yunnan southern geological survey engineering corporation;  
The structure of the mine is located in the north section of tanggula, changdu, lanping and simao fold, in the middle of the yunling fold belt and the central part of the jinsha river. In the area, the folds and faults are relatively developed, the geological structure is complex and the tectonic stress is more concentrated. The ore deposit type is the middle-low temperature hydrothermal copper polymetallic deposit. Chlorite, silicification, calcite, pyrite and carbonate are important signs to seek deposit.
【CateGory Index】: P618.2
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