摘要
本文通过对鸡冠嘴铜（铁）金矿床的地质特征及成矿机制的研究，认为该矿床明显受构造、地层和岩浆活动控制，在时空及成因上具有“一体多矿”、“一体多带”的成矿特点，为高。
As for the Jiguanzui Cu(Fe)-Au deposit, controlled clearly by structures, strata and magmatism, the ore bodiessurround small globular magmatic hotlies in time-space and genesis with the metallogenic features of one rock mass with multipleore bodies)) and )lone rock lusss with multiple beltsn. The geological characteristics is discussed and the origin approached.
出处
《矿产勘查》
1995年第2期77-82,69,共7页
Mineral Exploration
