索尔库都克铜钼矿地层构造及控矿因素

Stratigraphic structure and ore controlling factors of Saul Kedu copper molybdenum deposit

该矿地处新疆偏北方向的阿勒泰地区富蕴县管辖区域内,哈萨克斯坦板块以及西伯利亚板块二者相互结合部位是该矿大地构造位置所在。北塔山组(中泥盆统)第二亚组及乌伦古河组(第三系始-渐新统)是区内主要的地层出露,同时还发育风积层以及洪冲击层与残坡积层(第四系全新统)地层。构造在该区非常突出,控制该区矿体的空间展布。文中主要对该矿地层构造地层构造及控矿因素予以分析探讨,希望能对区内找矿工作提供参考。

This mine is located in the jurisdiction area of Fuyun County in Aletai area of Xinjiang in the direction of the north of Xinjiang. The combination of the Kazakhstan plate and the Siberia plate is the location of the geodetic structure of the mine. The second subgroup of the North Tashan formation （Middle Devonian） and the uuugu River Formation （third system beginning Oligocene） are the main strata in the region, while the aeolian layer, the flood impact layer and the residual plump layer （the Quaternary Holocene） are also developed. The structure is very prominent in this area and controls the spatial distribution of ore bodies in the area. This paper mainly analyzes and discusses the stratigraphic structure, stratigraphic structure and ore controlling factors in the mine, hoping to provide reference for the prospecting work in the area.