中条裂谷东延地段——王屋山地区铜矿成矿地质条件及找矿方向  

GEOLOGICAL CONDITION AND PROSPECTING DIRECTION OF COPPER MINERALIZATION IN EAST ZONE OF ZHONGTIAO RIFT——WANGWUSHAN MOUNTAINS,HENAN PROVINCE

作　　者：崔小军[1] 刘家军[2] 赵百胜[2] 杨东潮[1] 

机构地区：[1]河南省地质调查院,河南郑州450007 [2]中国地质大学地质过程与矿产资源国家重点实验室,北京100083

出　　处：《资源与产业》2006年第5期103-108,共6页Resources & Industries

基　　金：国家自然科学基金(40573026;40234051);国土资源大调查(200410200024)资助项目

摘　　要：研究对比了王屋山、中条山两地区的地层、岩性、构造、岩浆岩,认为王屋山地区与中条山地区同处于晚太古代—早、中元古中条裂谷中,经历了相同的地质演变过程,具有相似的成矿地质背景。确认王屋山地区具有良好的成矿地质条件和找矿前景,指出了该区今后的找矿方向。There is favorable geological condition and prospecting direction of copper mineralization in Wangwushan, Henan. It can be compared with the Tongchangyu and Hubu copper deposits in Zhongtiaoshan with respect to geological setting, host lithology, magma formation, tectonic form, and mineralization style. The perfect mineralization conditions include： the stepwise evolution of Zhongtiao rift; great mantle-connected fault supplying plenty of ore resource and place; frequent magma activity supplying heat energy and recruit ore matter; stripping fault system providing ore contain place; and mighty deformation and metamorphism reforming orebearing formation by activation and transference. The authors point out the prospecting conditions in the Wangwushan region.

关 键 词：河南王屋山 山西中条山 地质背景对比 成矿地质条件 找矿方向 

分 类 号：P618.41[天文地球—矿床学]