CAJ | 학술논문

托库孜达板—野狼沟地区分布于祁曼塔格成矿域西段,是白干湖成矿带的一部分,区内岩性主要为石炭系喀拉米兰河群火山岩,浅成岩及花岗岩广泛分布,又位于在阿尔金断裂带及昆中断裂带的交汇部位,两断裂的次一级在区内特别发育。从以往1/50万化探成果及1/5万遥感解译成果看,矿致异常在区内大面积分布。近年发现的野狼沟铜多金属矿于石炭系次火山岩及北西向断裂构造关系密切。所有地物化遥等特征都预示了该区良好的找矿前景。
탁고자체판—야랑구지구분포우기만탑격성광역서단,시백간호성광대적일부분,구내암성주요위석탄계객랍미란하군화산암,천성암급화강암엄범분포,우위우재아이금단렬대급곤중단렬대적교회부위,량단렬적차일급재구내특별발육。종이왕1/50만화탐성과급1/5만요감해역성과간,광치이상재구내대면적분포。근년발현적야랑구동다금속광우석탄계차화산암급북서향단렬구조관계밀절。소유지물화요등특정도예시료해구량호적조광전경。
Tuokuzidaban-Yelanggou area is located in the western part of Qimantage metallogenic megaprovince,which is one part of Baigan lake metallogenic belt.In the study area,the lithology mainly are the Carboniferous System Kalamilan river Group volcanic rock,hypabyssal rocks and granite distributed widely.It also located in the junction of Aerjin fracture zone and Kunzhong fracture zone,whose secondary fracture of the two fractures were specially developed.Based on the past 1：500 000 geochemical exploration achievements and 1：50 000 remote sensing results,anomalies related to mineralization are widely distributed in the study area,Yelanggou copper polymetallic mine,that discovered in recent years,is closely related with the Carboniferous System sub-volcanic rocks and NW strike fracture.All geochemical exploration and remote sensing features indicated good prospecting prospects.