摘要
蛇屋山金矿床是我国首先在湖北省发现并探明的大型红土型金矿床。矿床经渗流热卤水成矿作用,形成原生金矿化（体）；再经表生同化成矿作用形成风化型金矿床。矿床成因类型属渗流热卤水一表生成因的残积粘土型金矿床,工业类型为红土型金矿床。
Sheweishan gold deposit is a large-scale laterite-type deposit first found in Hubei Province of China.The deposit experienced vadose hot brine and formed original gold minerallization.And then through supergene weathering mineralllzation,weatheringtype gold deposit was formed.The deposit belongs to vadose hot brine-supergene genetic eluvial clay-type gold deposit and to laterite-type gold-deposit in terms of industry.
出处
《地质与勘探》
CAS
CSCD
北大核心
1996年第1期1-6,32,共7页
Geology and Exploration
关键词
金矿床
红土型
成矿
地质条件
形成机理
vadose hot brine
karst unconformity surface
barrier structure
weathering leaching
uncombined gold
lateritetype gold deposit.
