镇康章龙原生红土型金矿地质  

THE ORIGINAL AND LATERITIC GOLD DEPOSIT, ZHENKANG

作　　者：吴绍军 

机构地区：[1]云南地质矿产勘查开发局第四地质大队,云南保山678000

出　　处：《云南地质》2003年第3期281-287,共7页Yunnan Geology

摘　　要：章龙金矿既有原生型、又有红土型的共生金矿床。矿床受构造、地层、围岩制约。红土型金矿还受地形、残坡积层、风化壳发育程度影响。In Zhanglong Au orefield, there are the original and the associated lateritic Au deposits. The ore deosits are controlled by the structure, strata and wallrock. And the lateritic Au deposit is also influenced by the land form, eluvial-slope wash and weathering crust degvelopment.

关 键 词：金矿 地质 矿床类型 化探异常 红土化 矿床成因 镇康县章龙金矿区 

分 类 号：P618.51[天文地球—矿床学] P611[天文地球—地质学]