| 元阳采山坪铜矿矿床成因 |
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| 引用本文： | 张俊,刘晓燕,周德荣,廖镜明. 元阳采山坪铜矿矿床成因[J]. 云南地质, 2011, 30(3): 308-311 |
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| 作者姓名： | 张俊 刘晓燕 周德荣 廖镜明 |
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| 作者单位： | 云南省地质矿产勘查院玉溪地质矿产所,云南玉溪,653100 |
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| 摘 要： | 铜矿位于哀牢山推覆构造带上,含矿地层为哀牢山岩群凤港岩组,属火山—沉积变质铜矿,具有较好的地质成矿背景和地球化学成矿背景,找矿潜力大。
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| 关 键 词： | 火山—沉积变质 顺层产出铜矿 变粒岩层 凤港组第三段 云南元阳采山坪 |
THE GENESIS OF CAISHANPING CU DEPOSIT, YUANYANG |
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| ZHANG Jun,LIU Xiao-yan,ZHOU De-rong,LIAO Jing-ming. THE GENESIS OF CAISHANPING CU DEPOSIT, YUANYANG[J]. Yunnan Geology, 2011, 30(3): 308-311 |
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| Authors: | ZHANG Jun LIU Xiao-yan ZHOU De-rong LIAO Jing-ming |
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| Affiliation: | ZHANG Jun,LIU Xiao-yan,ZHOU De-rong,LIAO Jing-ming(Yuxi Institute of Geology & Mineral Resources,Yunnan Exploration Institute of Geology & Mineral Resources,Yuxi 653100) |
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| Abstract: | The Cu deposit is in the Ailaoshan nappe structural zone. The ore -bearing strata belong to Ailaoshan Group Fenggang rock formation. It is a volcano- sedimentary metamorphic Cu deposit. The Geological and Geochemical setting of Metallogenesis is good, with excellent prospecting potentiality. |
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| Keywords: | Volcano - Sedimentary Metamorphic Cu Deposit of Bedding Occurrence Granulite Bed Fenggang Formation Member 3 Caishanping,Yuanyang,Yunnan |
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