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我矿属汽化高温热液类以钨锰铁矿石为主的石英脉金属矿床,矿脉成组群产出于以张力为主的张剪力复合裂隙中。矿脉厚度平均为0.3～0.6公尺,倾角从72°～85°,于矿脉垂直及水平方向,呈有分枝、复合、膨大、缩小、尖灭等现象。成矿后,主要矿脉上盤一公尺至两公尺左右,有一组平行矿脉的破碎带,其宽度山4.0公尺至2.5公尺;另外一组断层大致与矿脉垂直,位移从几公分至数公寸,矿脉上盤与围岩接触处,有一层1公分到10公分的细泥,崩矿时,
My mineralization of high temperature hydrothermal tungsten wolframite-based quartz vein metal deposits, veins group into a group of tension-based tensile shear in the composite fracture. The average thickness of the veins is 0.3-0.6 meters, and the dip angle is from 72 ° to 85 °. The vertical and horizontal veins show branching, compounding, swelling, shrinking and pinching. After mineralization, the main veins on the plate from one meter to two meters, there is a group of parallel veins broken zone, the width of the mountain 4.0 meters to 2.5 meters; another set of faults roughly vertical with the veins, displacement from a few centimeters to Number of inches, the veins on the plate and the rock contact, there is a layer of 1 cm to 10 cm of fine mud, collapse,