| 腾冲滇滩铜厂山矽卡岩型铅锌矿床地质 |
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| 引用本文： | 何艳丽,李玲辉.腾冲滇滩铜厂山矽卡岩型铅锌矿床地质[J].云南地质,2009,28(2):152-156. |
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| 作者姓名： | 何艳丽 李玲辉 |
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| 作者单位： | 云南省地质矿产勘查院,云南,昆明,650051 |
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| 摘 要： | 铜厂山铅锌矿产于中酸性侵入岩与大东厂组碳酸盐岩接触带的矽卡岩中靠大理岩一侧和空树河组碎屑岩与大东厂组碳酸盐岩断层接触带中。矿区共发现5条铅锌矿体，其中规模较大具工业价值的有2条。
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| 关 键 词： | 铅锌矿体 矽卡岩型 控矿因素 铜厂山 云南腾冲滇滩 |
THE GEOLOGY OF TONGCHANGSHAN SKARN PB-ZN DEPOSIT OF DIANTAN, TENGCHONG |
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| HE Yan-li,LI Ling-hui.THE GEOLOGY OF TONGCHANGSHAN SKARN PB-ZN DEPOSIT OF DIANTAN, TENGCHONG[J].Yunnan Geology,2009,28(2):152-156. |
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| Authors: | HE Yan-li LI Ling-hui |
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| Institution: | ( Yunnan Exploration Institute of Geology ＆ Mineral Resources, Kunming 650051 ) |
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| Abstract: | The Tongchangshan Pb - Zn deposit is formed in the skam of contact between the intermidiate - acid intrusive rock and the Dadongehang Formation carbonate rock, which is more adjacent to the marble side, and in the fault contact between Kongshuhe Formation clastic rock and Dadongchang Formation carbonate rock. There are 5 Pb -Zn ore bodies discovered in this orefield, including 2 ore bodies with large scale and commercial value. |
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