摘要
矿体产于中三叠统上兰组上段第一层层间裂隙和破碎带。上兰组与其上的攀天阁组属"双峰式"火山岩。地层层位、热液运移和矿质沉淀的构造空间控制了本矿床的产出。属典型的中—高温热液型铜铅锌多金属矿床。
The ore body is in the inter - bed fissure and fracture zone of Middle Triassic Shanglan Formation Upper Member 1^st bed. The Shanglan Formation and the superincumbent Pantiange Formation belong to the ＂2 - peak＂ volcanic rock. The stratigraphic horizon, hydrothermal migration and ore precipitation structure space control the formation of this ore deposit, which is a typical mid high T hydrothermal Cu - Pb - Zn multimetaUic deposit.
出处
《云南地质》
2011年第1期32-37,共6页
Yunnan Geology
关键词
中—高温热液型
铜铅锌多金属矿
上兰组上段赋矿
“双峰式”火山岩
云南德钦鲁春
High T Hydrothermal Type
Cu -Pb -Zn Multimetallic Deposit
Ore -Bearing Shanglan Formation Upper Member
＂2 - Peak＂ Volcanic Rock
Luchun, Deqin, Yunnan
