中条山西南段与变基性岩有关的铜矿地质特征及成因浅析  

Geological Features of Cu Deposits Related to the Metamorphic Basic Rock and Its Origin in Southwestern Zhongtiao Mountain

作　　者：薛克勤[1] 赵月凤 董清雷 

机构地区：[1]山西省地质调查院 [2]山西省岩石矿物测试应用研究所,太原030001

出　　处：《前寒武纪研究进展》2002年第3期151-159,共9页Progress in Precambrian Research

基　　金：中国地质调查局"华北地台成矿规律和找矿方向综合研究项目"(编号 :2 0 0 110 2 0 0 0 38)

摘　　要：与变基性岩有关的铜矿 ,是在中条山西南段新发现的一种新的铜矿类型 ,其形成是在原始基性岩浆侵入或喷发作用形成的矿源岩或矿化体基础上 ,经过区域变质和印支 -燕山期构造 -岩浆热液的改造加富而成 ,其成因应属与变基性岩有关的变质 -热液改造型铜 (镍、铁 )矿床。The Cu deposits related to metamoephic basic rock is a new type of Cu ore deposit discoveried in Southwestern Zhongtiao Mts. The authors think that the Cu ore deposits in the area are the products of normal metamorphic activities and structural-magmatic in Indosinian-Yanshan orogeny after basic vein and basic volcanic rock with plentiful Cu (Ni ,Fe) mineral matter occurred. The type of the deposit is Cu (Ni,Fe) ore deposit remodeled by metamorphism and hydrothermal related to metamoephic basic rock.

关 键 词：变基性岩 中条山 铜矿床 成矿作用 成因 喷发作用 

分 类 号：P618.41[天文地球—矿床学]