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块状硫化物矿床地质地球化学特征与形成机理
引用本文:刘晓东,周涛发.块状硫化物矿床地质地球化学特征与形成机理[J].合肥工业大学学报(自然科学版),1999(4).
作者姓名:刘晓东  周涛发
作者单位:合肥工业大学资源与环境科学系
摘    要:块状硫化物矿床可分为VMS和SEDEX矿床两大类。文章从赋矿岩石、成矿时代、控矿构造背景、矿石组分、矿化与蚀变等方面总结了两大类矿床的主要地质特征,从成矿流体性质、微量元素、硫同位素和铅同位素等方面总结了两类矿床流体成矿系统主要地球化学特征,论述了块状硫化物矿床的形成机理。

关 键 词:块状硫化物矿床  VMS  SEDEX  矿床地质地球化学  流体成矿系统  成矿机理

General geological and geochemical characteristics and ore forming mechanism of the massive sulfide deposits
LIU Xiao dong,ZHOU Tao fa.General geological and geochemical characteristics and ore forming mechanism of the massive sulfide deposits[J].Journal of Hefei University of Technology(Natural Science),1999(4).
Authors:LIU Xiao dong  ZHOU Tao fa
Abstract:The massive sulfide deposits are divided into two types: the volcanic hosted massive sulfide deposits (VMS) and the sedimentary hosted deposits of exhalation (SEDEX). General geological and geochemical characteristics of VMS and SEDEX are discussed in terms of the host rocks, the formation time and tectonic settings, mineralization and alterations and the composition of ore forming fluid system, trace elements and the S, Pb isotopes , and the ore forming mechanisms of the VMS and SEDEX are stated in this paper.
Keywords:the massive sulfide deposits  VMS  SEDEX  geological and geochemical characteristics  fluid ore  forming system  ore  forming mechanism  
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