摘要
云南省富宁县地处中国著名的"滇黔桂金三角"微细粒浸染型金矿成矿区,是我国重要的金矿产地之一。水合口金矿属于文山-富宁成矿带,赋矿层位不固定,具有多层性,主要含矿层位有三叠系、泥盆系以及寒武系。赋矿岩性主要为一套细粒碎屑岩-泥质岩-碳酸盐岩组合。构造在很大程度上决定了水合口金矿床的时空分布和成因。
Funing County,Yunnan Province is located in China's famous"Dianqiangui Golden Triangle"fine-grained disseminated gold deposit metallogenic area and is one of China's important gold deposits area.The Shuihekou gold deposit belongs to the Wenshan-Funing metallogenic belt.The ore-bearing strata are not fixed and have multiple layers.The main ore-bearing strata are Triassic,Devonian,and Cambrian.Ore-bearing lithology is mainly a set of fine grained detrital rock、argillaceous rock、carbonate rocks combination.To a large extent,the structure determines the spatial and temporal distribution and genesis of the Shuihekou gold deposit.
作者
苏红中
SU Hong-zhong(Yunnan Metallurgical Resources Co.,Ltd.,Kunming 650216,China)
出处
《世界有色金属》
2020年第10期119-120,共2页
World Nonferrous Metals
关键词
水合口金矿
地质特征
控矿因素
Shuikou gold deposit
geological characteristics
ore control factors
