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“层控式”矽卡岩矿床特征及成矿机制——以铜陵大团山铜(金)矿床为例
引用本文:凌其聪,周贵斌,黄许陈,颜玉琴.“层控式”矽卡岩矿床特征及成矿机制——以铜陵大团山铜(金)矿床为例[J].地质与资源,1998,7(2):91.
作者姓名:凌其聪  周贵斌  黄许陈  颜玉琴
作者单位:1. 中国地质大学, 武汉;2. 安徽狮子山 铜矿;3. 安徽地矿局 321地质队
摘    要:层控式矽卡岩矿床中的矽卡岩和矿体主要顺地层呈似层状或透镜状产出,其矿物组合及矿物特征与一般的矽卡岩类似。成矿控制因素主要是地层层位、岩性和层间滑脱空间。成矿过程也分为矽卡岩期和石英硫化物期两期,成矿温度可高达390℃,其主要成矿机制是源自岩浆的热液沿层间发生渗滤扩散交代作用。

关 键 词:层控式  矽卡岩  铜金矿床  成矿机理  安徽铜陵  
收稿时间:1997-10-24

MECHANISM AND THE CHARACTERISTICS OF STRATABOUNDTYPE ORE DEPOSIT
Ling Qicong,Zhou Guibin,Huang Xuchen,Yan Yuqin.MECHANISM AND THE CHARACTERISTICS OF STRATABOUNDTYPE ORE DEPOSIT[J].Geology and Resources,1998,7(2):91.
Authors:Ling Qicong  Zhou Guibin  Huang Xuchen  Yan Yuqin
Institution:1. China University of Geosciences, Wuhan;2. Shizishan Copper Mine, Anhui;3. No.321 Geological team, Anhui Bureau of Geology and Mineral Resources
Abstract:he stratabound type skarn ore deposits are commonly seen in Tongling,Anhui Province.As an example,Datuanshan CuAu ore deposit is discussed in the paper.The characteristics of this kind of ore deposit that are different from common skarn one are as follow:(1)The skarn and ore bodies occur along the strata of the country rock as mainly quasistratiform .No alteration zoning between skarn and magmatic rocks can be seen as that in common skarn.(2)The major factors controlling oreforming processes are strata,lithology,magmatic rock and detachment among strata.(3)The oreforming mechanism is infiltrationdiffusion metasomatism.Other characteristics such as mineral assemblages,oreforming stages and temperature,salinity of oreforming fluid,etc.,are similar to those of common skarn ore deposits.
Keywords:stratabound type skarn  CuAu ore deposit  oreforming mechanism  Tongling  Augui Provines
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