湖南省界牌矽卡型铜钨矿地质特征及控矿条件  

Geological Characteristics and Ore-controlling Conditions of skarn type Copper-Tungsten Deposits in Jiepai Area,Hunan Province

作　　者：胡可卫 董富权[1] 黄荣才[1] 

机构地区：[1]中国人民武装警察部队黄金第11支队,湖南宁乡410600

出　　处：《矿产与地质》2011年第3期189-192,共4页Mineral Resources and Geology

摘　　要：界牌矽卡型铜钨矿位于南岭成矿带内越城岭NNE向构造带铺里-界牌断裂南段西侧,为一典型的矽卡岩铜钨矿床。通过对该矿床的地质特征、地球化学特征及控矿条件分析研究表明,该矿床受构造断裂控制,容矿岩石主要为寒武系上统下段碳酸盐岩及少量花岗岩,在时空上可能与燕山期侵入活动密切相关。Jiepai deposit is a skarn-type copper and tungsten deposit in Jiepai Area,Xinning County,Hunan Province,which lies in Puli-Jiepai fault's southern part on western side of Yuechengling NNE-striking tectonic zone in the Nanling metallogenic belt.Research on the geological characteristics,soil geochemical characteristics and ore-controlling conditions indicates that the deposit is mainly controlled by the structural fault belt.The mineralization is held by lower Cambrian carbonate on the lower stage and less granites.It is probably related to the Yanshanian magma intrusion in time and space.

关 键 词：矽卡岩铜钨矿床 铺里-界牌断裂 土壤地球化学特征 控矿条件 

分 类 号：P5[天文地球—地质学]