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一、矿床地质特征矿区位于“雪峰古陆”西缘.汞矿带主要受北东、北北东向华夏、新华夏构造控制.各矿田大多分布在北东、北北东向之大背斜轴部或近轴部,并受背斜上的纵向张断裂或压扭性断裂控制.矿田中的矿床往往同时受与北东、北北东向纵向张性(或压扭性)断裂斜交的一组北东东-东西向张扭性断裂控制.矿床多位于相交的二组构造之北东象限“锐角区”.矿体常沿北西西、北西向次级断裂和褶皱产出,少数沿北北东、北东东向分布.华夏、新华夏系二、三级以至
First, the geological characteristics of the deposit Mine is located in the western edge of the “Xuefeng ancient land.” Mercury ore belt is mainly controlled by the structure of the North East and North-East to the Cathaysia and the New China. Most of the ore fields are distributed in the north east and north north east Of the large anticlinal axis or near the axis, and by the anticlinal longitudinal Zhang Zhang fracture or compression-shear fracture control ore deposits often at the same time with the North East, North-East longitudinal tensile (or compression ) A series of NE-EW-TST shear-skewed faults controlled by a series of faults.The orebodies are mostly located in the NEQ / “acute angle zone” of the two intersecting structures.The orebodies are often distributed along the northwestern and western NW secondary faults And fold output, a small number of distribution along the North, East, North East east China and the New China two, three and even