探讨松树沟铜矿矿床地质特征及矿床成因

Geological characteristics and genesis of the ore deposit of the pine gully copper deposit

松树沟铜矿位于伊犁地块东缘,阿吾拉勒铜多金属成矿带内。矿区位于伊利地块、阿吾拉勒晚古生代裂谷系东缘,处于区域上的玉希莫洛该达坂-巴腊陶NW向构造带上,成矿区带划分属阿吾勒铁铜成矿带东延部分。成矿地质条件优越。断裂构造发育,岩浆活动频繁。文中笔者在对该矿地质特征进行分析的基础上,探讨其矿床成因,以期为该区找矿提供参考。

The Songshugou copper deposit is located in the east of Yili massif, the copper polymetallic metallogenic belt. The mine is located in Erie, the plots of Late Paleozoic rift system in the area of the eastern margin, jade and Mo Luo the Dabancheng - Bala Tao NW trending tectonic belt, metallogenic belts of awil Fe Cu metallogenic belt eastward extension. The metallogenic geological conditions are superior. Fracture structure is developed and magmatic activity is frequent. In this paper, based on the analysis of the geological characteristics of the mine, the genesis of the ore deposit is discussed in order to provide reference for the prospecting in this area.