湖南溆浦县陶金坪金矿地质特征及成因探讨  

Geological Characteristics and Genesis of the Taojinping Au Deposit in Xupu,Hunan

作　　者：郭方方[1] 袁跃清 王万军[3] 

机构地区：[1]河南理工大学,河南焦作454003 [2]河南有色金属地质矿产局第一地质大队,河南安阳455000 [3]海南省地矿局,海口570206

出　　处：《四川地质学报》2009年第3期284-287,共4页Acta Geologica Sichuan

摘　　要：陶金坪金矿床位于雪峰山脉中段,矿化体赋存于新元古界板溪群的粉砂质板岩中,矿化富集主要受构造控制。文章阐述了陶金坪金矿床成矿地质背景,矿床(体)地质特征,探讨了成矿物质来源、矿床成因,指出了今后的找矿方向。The Taojinping Au deposit is located in the middle part of the Xuefeng Mountains.Stratiform mineralized bodies occur in silty slate of the Neoproterozoic Banxi Group.The Au mineralization is mainly controlled by structure.The present paper deals with geological setting,geological features,ore material sources and ore genesis of the Taojinping Au deposit and makes an approach to the range of reconnaissance for the deposit.

关 键 词：陶金坪金矿床 找矿方向 湖南涂又浦 

分 类 号：P618.51[天文地球—矿床学]