新疆皮山县喀瓦克铜矿矿床地质特征及找矿前景分析  

Geological Features and Prospecting Prospect of the Kawake Cu Deposit in Pishan,Xinjiang

作　　者：袁兆平[1] 张建秋 曾勇[1] 陈思尧 YUAN Zhao-ping;ZHANG Jian-qiu;ZENG Yong;CHEN Si-yao(Regional Geological Surveying Team,BGEEMRSP,Chengdu 610213)

机构地区：[1]四川省地质矿产勘查开发局区域地质调查队,成都610213

出　　处：《四川地质学报》2021年第S01期68-73,共6页Acta Geologica Sichuan

基　　金：新疆维吾尔自治区国土资源厅“新疆皮山县喀瓦克一带铜矿调查评价”(项目编号:KL15-2-LQ18)。

摘　　要：新疆皮山县喀瓦克铜矿位于西昆仑北缘古生代复合沟弧带,是北昆仑库尔良地区较为典型的与基性岩有关的铜(镍)硫化物矿床。通过调查评价工作,目前矿区内已圈定了5条铜矿(化)体,铜矿(化)体长100~2300 m,铜平均品位0.3%~0.74%之间,厚度1.6~2.36 m不等。该铜矿区成矿地质条件有利,成矿区位优越,化探成果显示有利,矿化显示较好,找矿前景良好。The Kawake Cu deposit in Pishan,Xinjiang lies in the northern section of the Paleozoic composite trench-arc zone on the northern margin of west Kunlun Mts.and is one typical Cu-Ni sulfide deposit related to basic intrusive in the Kuerliang region,north Kunlun Mts.Five Cu-mineralized bodies are delineated.The Cu-mineralized bodies are 100-2300 m long with average grade of 0.3-0.74%Cu and thickness of 1.6-2.36 m.The ore-forming geological conditions in the ore district are excellent,and the prospecting prospect is good.

关 键 词：喀瓦克 铜矿 矿床地质特征 找矿前景 

分 类 号：P612[天文地球—矿床学]