中条山地区地壳递进演化与胡─篦型铜矿床的成因  

PROGRESSIVE EVOLUTION OF CRUST AND GENESIS OF “HU BI” TYPE COPPER DEPOSITS IN ZHONGTIAOSHAN DISTRICT

作　　者：刘亮明[1] 陈国达[1] 彭省临[1] 杨牧[1] 

机构地区：[1]中南工业大学地洼学说成矿学研究所

出　　处：《中南工业大学学报》1999年第4期352-358,共7页Journal of Central South University of Technology(Natural Science)

基　　金：国家自然科学基金;国家教育部博士点基金

摘　　要：通过分析中条山地区的沉积建造、岩浆建造、变质作用和构造型相等对中条山地区地壳演化运动史进行了反演，并用地洼学说的递进成矿思想对胡篦型铜矿床的成因特征进行了全面分析，论证了中条山地区地壳经历了地槽、地台和地洼３个不同性质的大地构造阶段，胡篦型铜矿床是经中条期裂谷环境的喷流沉积成矿作用、中条褶皱造山运动时的变形变质改造成矿作用和西洋河期再生裂谷环境中的热液叠加成矿作用而形成的多因复成矿床．The progressive evolution history of crust is deduced by analyzing sedmentary formation, magmatic formation, metamorphism and structure style in Zhongtiaoshan district, and the genetic features of “Hu Bi” type copper deposits are thoroughly analyzed by using the progressively metallogenic thought of Diwa theory. The crust in Zhongtiaoshan district has undergone 3 different geotectonic stages which are geosyncline, platform and Diwa. The “Hu Bi” type copper deposits are compounded polygeneticcally, by compounding of exhalative sedmentary mineralization in rift of Zhongtiao Period, reforming mineralization in deformation and metamorphism of Zhongtiao Orogeny, and hydrothermal mineralization in rerifting setting of Xiyanghe Period.

关 键 词：地壳演化 成矿作用 胡-篦型铜矿床 中条山 

分 类 号：P618.410.1[天文地球—矿床学]