摘要
介绍了镜铁山式铜矿床的地质特征 ,分析了其成因 ,并对其形成过程进行理论推导。认为该矿床为与火山作用有关的中—低温热液改造层控矿床。
Geological characteistics of Jingtie Mountain's copper deposit was introduced. It's origin and formation processes are analysised. Huashugou copper deposit is believed to be a midle-low temperature hydrothermal reworked stratabound deposit relating to volcanic action.
出处
《地质与勘探》
CAS
CSCD
北大核心
2000年第5期15-19,共5页
Geology and Exploration
关键词
地质特征
热液改造
层控铜矿床
镜铁山
copper deposit, geological characteristics, hydrothermal rework, stratabound deposit, formation processes, Jingtie Mountain
