| 腾冲老厂坪子地区铜多金属矿 |
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| 引用本文： | 谢永富.腾冲老厂坪子地区铜多金属矿[J].云南地质,2004,23(3):351-361. |
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| 作者姓名： | 谢永富 |
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| 作者单位： | 云南地矿资源股份有限公司保山分公司,云南,保山,678000 |
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| 摘 要： | 老厂坪子地区已发现十余个矿床(点),矿体赋存于花岗岩与碳酸盐岩接触带及其附近的断裂破碎带中,并受其双重控制。矿石品位较富,矽卡岩型和热液型成因,矿质来源于二叠系、三叠系碳酸盐岩及燕山早期岩浆岩。
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| 关 键 词： | 铜多金属矿床 双重控矿 老厂坪子地区 腾冲云南 |
| 文章编号： | 1004-1885(2004)03-351-11 |
THE LAOCHANGPINGZI COPPER MULTIMETALLIC DEPOSIT, TENGCHONG |
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| XIE Yong-fu.THE LAOCHANGPINGZI COPPER MULTIMETALLIC DEPOSIT, TENGCHONG[J].Yunnan Geology,2004,23(3):351-361. |
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| Authors: | XIE Yong-fu |
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| Abstract: | There are more than 10 ore deposits(occurrences) discovered in Laochangpingzi area. The orebodies are distributed in the fault-fissure belt in or nearing the contact between granit and carbonate rock and controlled by them. The ore grade is high. The genesis belongs to skarn type and hydrothermal type. The metallogenetic materal is originated from Permian, Triassic carbonatc rock and early Yanshanian magmatic rock. |
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| Keywords: | Cu Multimetallic Deposit Dual Confrolling Laochangpingzi Area Tengchong Yunnan |
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