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。
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.
出处
《云南地质》
2011年第3期308-311,共4页
Yunnan Geology
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
Volcano - Sedimentary Metamorphic
Cu Deposit of Bedding Occurrence
Granulite Bed
Fenggang Formation Member 3
Caishanping, Yuanyang, Yunnan
