青海东昆仑拉陵灶火矿区地质特征及找矿远景

Pull the geological characteristics and prospecting of mine fire Ling Qinghai East Kunlun

拉陵灶火位于东昆仑西段北坡,青海柴达木盆地南缘,地质沉积岩石为祁漫塔格蛇绿混杂岩,有著名的东昆北深大断裂处于矿中间,主要呈现区域构造―地层、构造―岩浆带及矿产的分布格局。本文通过分析拉陵灶火地区地质特征,按照矿产区域物化探异常分布、矿床时空分布规律,探析了其找矿远景及后期找矿方向。

Located in the western section of the East Kunlun Ling Zaohuo the north slope of the southern margin of Qinghai Qaidam Basin, the geological sedimentary rock Qimantag OPHIOLITIC MELANGE, the famous East North Queensland deep fault in mine, the distribution pattern shows the main tectonic stratigraphic and tectonic - magmatic belt, and minerals. In this paper, through the analysis of the geological characteristics of Ling Zaohuo pull area, according to mineral regional geophysical and geochemical anomaly distribution, temporal and spatial distribution of the ore deposits, ore prospecting and post ore ProsPecting direction.