探讨新疆阿希金矿矿床地质特征及矿床成因  

Discussion on geological characteristics and ore genesis of Xinjiang gold deposit in Axi

作　　者：李龙 

机构地区：[1]新疆地矿局第二区调大队,新疆昌吉831100

出　　处：《世界有色金属》2017年第22期176-177,共2页World Nonferrous Metals

摘　　要：阿希金矿位于伊利-中天山板块北缘博罗霍洛岛弧带的吐拉苏盆地中,南北分别以NWW向的伊利盆地北缘断裂和科古琴山南坡断裂为界。下石炭统大哈拉军山组第五岩性和阿恰勒河第一岩性段在区内广泛出露,断裂构造发育。本文对阿希金矿地质特征及矿床成因进行详细研究,旨在为该区找矿工作提供参考。The Axi Gold Deposit is located in the northern Boluo Yili Central Tianshan plate Holloway island arc zone Tulasu basin, North and south respectively by NWW to the Yili Basin and mountain Keguqin Nanpo fault fault as the boundary. The lower Carboniferous Dahalajunshan formation lithology and fifth Aqiale river the first lithologic section are widely exposed in the region, faults. This paper make a detailed research on the geological characteristics and genesis of gold deposit in Axi, in order to provide reference for the work of the prospecting area.

关 键 词：阿希金矿 地质特征 矿床成因 

分 类 号：P618.51[天文地球—矿床学]