摘要
老集寨矿区位于哀牢山地体的南端,矿体主要赋存于三叠系高山寨组第二段(T_3g^2)中北西向的层间构造破碎带内。北西向的金竹寨—老集寨断裂(F3)即为导矿构造也为容矿构造,呈北东—南西走向的依里断裂(F_5)为破矿构造。
Laojizhai orefield is on the S end of Ailaoshan geological terrain. The orebody is mainly in the NW interbedded structural fractured zone of T Gaoshanzhai Formation Member ⅱ. The NW Jinzhuzhai- Laojizhai fault（ F_3） is either the ore- transmission or ore- container structure. The NE- SW Yili fault（ F_5） is the ore- break structure.
出处
《云南地质》
2015年第4期503-507,共5页
Yunnan Geology
关键词
层间破碎带
导矿构造
容矿构造
破矿构造
云南金平老集寨
Interbedded Fractured Zone
Ore-Transmission Structure
Ore-Container Structure
Ore Break Structure
Laojizhai
Jinping
Yunnan
