新疆克峡希地区铜矿化地质特征及成因浅析  

Characteristics and Cause Analysis of Copper Mineralization Geology in Kexiaxi Region of Xinjiang

作　　者：庞星 陈黎昀[1] 梁世川 

机构地区：[1]核工业二一六大队,新疆乌鲁木齐830011 [2]新疆维吾尔自治区地质环境监测院,新疆乌鲁木齐830000

出　　处：《能源与节能》2015年第5期98-100,共3页Energy and Energy Conservation

摘　　要：叙述了克峡希铜矿的地质构造、矿化特征及成矿原因。矿石矿物简单,包括硫化矿石矿物、氧化矿石矿物和自然金属矿物三种。以强烈的碳酸盐化、黄铁矿化、绿泥石化、硅化、孔雀石化、绢云母化为特征。由此推断克峡希铜矿属复合成因的斑岩铜矿床,以此为背景进行地质特征及成因调查。Described the geological structure, mineralization characteristics and metallogenic genesis of the Kexiaxi Copper. Ore minerals are simple, including sulphide ore minerals, oxide ore minerals and natural metal oxide ore mineral. The characteristics of this copper mineralization are strong carbonation, pyritization, chloritization, silicification, peacock petrochemical, and sericitization. It can be seen that Kexiaxi copper mineralization is the genus porphyry copper deposit with complex causes, and the geological characteristics and causes of the investigation were made.

关 键 词：克峡希 矿床地质 成矿时代 矿床成因 

分 类 号：F407.1[经济管理—产业经济]