摘要
矿体似层状、透镜状赋存于中寒武系田蓬组碳酸盐岩岩系中,北东向褶皱的滑脱空间、断裂破碎带为容矿的重要场所。
The stratoid, lenticular ore bodies are in Middle Cambrian Tianpeng Formation carbonate rock se- ties. And the sliding space of NE - ward fold and fault fractured zone are the important ore - bearing places.
出处
《云南地质》
2011年第3期305-307,288,共4页
Yunnan Geology
关键词
多阶段多成因
原始沉积矿源层
层间滑脱带
含矿热液深循环
云南麻栗坡
Muhi- Stage ＆ Multi -Genesis
Original Sedimentary Ore -Source Bed
Intrabed SlidingZone
Circle of Ore - Bearing Thermal Fluid
Malipo, Yunnan
