Genesis and district mineralization model of lead-zincdeposits from the eastern margin of Kangdian axis

机译：康迪安东部缘铅锌矿泉矿石的成因与区矿化模型

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Situated on the eastern margin of Kangdian axis the lead-zinc mineral belt is an important mineral occurrence of lead-zinc in southwestern China. It is 1 200 km in length from Kangding in Sichuan Province to northeastern Yunnan Province, and 500 km in width from west to east. There are four large deposits, fourteen middle deposits and many small deposits or mineralized spots. Famous large deposits such as Doliangzi, Tianbaoshan, Chipu and Kuangshanchang are distributed in this belt.

机译：位于康迪安轴的东部缘，铅锌矿皮带是中国西南部铅锌的重要矿物发生。距离四川省东北部的康达省为康达200公里，从西向东宽500公里。有四个大型沉积物，十四个中间沉积物和许多小沉积物或矿化点。着名的大型存款，如Doliangzi，Tianbaoshan，Chipu和kuangshanchang分布在此腰带中。

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《Internatioanl symposium on epithermal (low-temperature) mineralization》|1999年||共3页
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GUAN Shiping; LI Zhongxiong;
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中图分类矿床成因;
关键词
genesis; district mineralization model; lead-zinc deposits; Kangdian axis;

机译：创世纪;区矿化模型;铅锌矿床;康迪轴;

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Genesis and district mineralization model of lead-zincdeposits from the eastern margin of Kangdian axis

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