新疆伊吾县绿源金矿地质特征及成因初探  

The Preliminary Study on the Geological Characteristics and Genesis of the Lvyuan Gold Deposit in Yiwu County,Xinjiang

作　　者：张佳儒[1] 邓刚[1] 贾红旭[1] 陈疆[1] 张建恩[1] 夏毅[1] 张子蛟[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第六地质大队,新疆哈密839000

出　　处：《新疆地质》2016年第4期491-495,共5页Xinjiang Geology

基　　金：新疆地质矿产勘查开发局第六地质大队自筹资金新疆伊吾县绿源金矿预普查项目资助

摘　　要：绿源金矿位于准噶尔微板块东部三塘湖晚古生代弧间盆地内,为近年来新发现的小型金矿床。该金矿床产于上石炭统巴塔玛依内山组陆相火山岩NE向断裂构造带中,局部地段金矿层较富集。通过矿床地质特征对比研究分析,初步认为该矿床成因类型属浅成低温热液型金矿床,找矿前景较好。The lvyuan gold deposit is located in Neopaleozoic Santanghu interarc basin,it is a small gold deposit that discovered by geologists.The gold deposit formed in continental volcanics of Upper Carboniferous batamayineishan formation,and it is controlled by NE direction fault.part of the deposit has high gold content.Through research of geological characteristics of the deposit,it is considered that the genetic type of the deposit belongs to hypabyssal hydrothermal gold deposit and the prospect ofprospection is good.

关 键 词：新疆 伊吾县 绿源金矿 地质特征 成因初探 

分 类 号：P618.51[天文地球—矿床学]