新疆轮台县阿切克他什磁铁矿床地质特征及成因分析  

Geological Characteristics and Genesis Analysis of the Aqieketashi Magnetite Iron Deposit in Luntai County, Xinjiang

作　　者：张海军[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第三地质大队,新疆库尔勒841000

出　　处：《资源导刊（地球科技版）》2014年第3期15-17,共3页

摘　　要：新疆轮台县阿切克他什磁铁矿床位于轮台县哈尔克山科克铁克一带，矿床产于下泥盆统的下部片理化泥质灰岩之上、中部绿泥石化长英质变砂岩之下的矽卡岩带中。矿床由7个矿体组成，矿石矿物为磁铁矿，脉石矿物为绿泥石，矿物共生组合为磁铁矿-绿泥石。矿石构造以致密块状为主，其次是浸染状。矿床成因属于高温热液交代型。断层构造、矽卡岩带及花岗岩可以作为找矿标志。在区域上具有寻找同类型矿床的前景。The Aqieketashi magnetite iron deposit in Luntai County is located in the Keketieke zone of the Haerke Mountain. The ore-bearing rock series are belongs to skarn zone which is made up of foliated argillaceous limestones in the Lower Devonian. The deposit is consisting of seven ore bodies. The main ingredient of the ores is magnetite, accompanying soapstone and sphene. The main structure of ores is dense massive, the second is impregnated. Genesis belongs to the high temperature hydrothermal metasomatic type. Fault structure, skarn zone and granite can be used as prospecting marks, which has the prospect of looking for the same type deposits in the area.

关 键 词：地质特征 矿床成因 阿切克他什磁铁矿床 新疆轮台县 

分 类 号：P618.51[天文地球—矿床学]