摘要
近年来,对于块状硫化物矿床地质特征和成因模式的研究,在其矿化分带、下盘矿化和蚀变,不同矿床类型共生关系、后期变质改造、区域控矿因素、成矿地质背景、成矿物质和成矿溶液来源、成矿溶液性质、矿石沉淀机制、以及现代成矿作用等方面都有重要进展,本文对这些进展作了简要综述.
With regard to the geologic features and the genetic models of massive sulphide deposits, advances of researeh have been made in recent years. Several respects such as metal zonations, footwall alterations, regional constraints on ore localization, geological settings during ore formation, sources of ore materials and fluids, mechanisms of ore precipitation, and the modern analogues of these deposits are presented.
出处
《地质科技情报》
CAS
CSCD
北大核心
1989年第2期67-73,共7页
Geological Science and Technology Information
