九瑞区大城门—仙姑台斑岩型铜矿成矿地质条件  

THE METALLOGENETIC GEOLOGIC CONDITIONS OF DACHENGMEN-XIANGUTAI PORPHYRY CU DEPOSIT IN JIURUI AREA

作　　者：赵胜利[1] 秦润君[1] 曹其琛[1] 臧进前[1] 

机构地区：[1]桂林理工大学地球科学学院,广西桂林541004

出　　处：《云南地质》2012年第4期518-522,共5页Yunnan Geology

摘　　要：大城门地区斑岩型铜矿与燕山期深源浅成中酸性杂岩体相关,成矿与断裂、围岩性质、岩浆活动控制,认为深部与边缘仍有较大找矿潜力,是理想的找矿空间。The porphyry Cu deposit of Dachengmen area is in relation with Yanshanian typhonic hypabyssal intermediate - acid complex. And the metallogenesis is related to the fault, lithologic character of wall rock and magmafic activity. We believe the prospecting potentiality is still rather good in the deep and marginal area, which are the ideal prospecting space.

关 键 词：斑岩型铜多金属 构造岩浆岩控矿 燕山期杂岩 深度找矿潜力 江西九瑞地区 

分 类 号：P618.41[天文地球—矿床学] P612[天文地球—地质学]