青海省卡尔却卡北铜多金属矿地质特征及矿床成因分析

Geological characteristics and genesis of the kalqueka North copper polymetallic deposit,Qinghai Province

卡尔却卡北铜多金属矿位于柴达木盆地西南缘那陵格勒河上游南岸。区域地层出露较简单,岩浆活动极为强烈,以中~酸性侵入岩为主,基性、超基性岩浆活动及火山活动很微弱,构造以断裂为主,本区经历了多次复杂而强烈的构造运动。本文对青海省格尔木市卡尔却卡北铜多金属矿地质特征及找矿远景进行了分析探讨。

The North copper polymetallic deposit of karqueka is located in the South Bank of the upper reaches of nalinggol River on the southwest edge of Qaidam Basin.The regional strata are relatively simple in outcropping,with extremely strong magmatic activity,dominated by medium acid intrusive rocks,weak basic and ultrabasic magmatic activities and volcanic activities,and dominated by faults.The region has experienced many complex and strong structural movements.In this paper,the geological characteristics and prospecting prospect of kalqueka copper polymetallic deposit in Golmud City,Qinghai Province are discussed.