云南镇沅县和平丫口金矿地质特征  

THE GEOLOGICAL FEATURE OF HEPINGYAKOU AU DEPOSIT IN ZHENYUAN,YUNNAN

作　　者：卢玉喜 易丙红 

机构地区：[1]云南省地质调查院,云南昆明650216

出　　处：《云南地质》2016年第2期204-208,共5页Yunnan Geology

摘　　要：矿床分布于九甲-墨江断裂带中,单个矿体产于F_1、F_2两断裂所夹持的上古生界浅变质沉积岩系与南西侧浪泥塘-麻子村超基性岩体的接触带附近,矿体严格受断裂(F_1、F_2)控制,其规模、形态、产状随断层规模和产状变化而变化;矿床成因类型属构造蚀变岩型中低温热液金矿床。The ore deposit is in Jiujia-Mojiang fault zone. The individual ore body is near the contact of Upper Palaeozoic epimetamorphic sedimentary rock series between F1, F2 and SW Langnitang-Mazicun uhrabasic rock body. The ore body is strictly controlled by F1, F2. The scale, form and occurrence of ore body change following those of the faults. It belongs to structural aherated rock middle-low T hydrothermal Au deposit in genesis.

关 键 词：断裂控矿 构造蚀变 热液矿床 云南镇沅和平丫口 

分 类 号：P618.51[天文地球—矿床学]