摘要
505脉总体走向270~310°,呈透镜体状、扁豆状以尖灭再现或尖灭侧现的形式产出.505脉为一典型的具多金属硫化物含金石英脉.含金矿物主要是黄铁矿,其次为方铅矿和黄铜矿.黄铁绢英岩化是金矿化的重要标志.控矿构造有4次脉动,与其对应,505脉分4个成矿阶段,主要是Ⅰ、Ⅱ阶段及Ⅰ、Ⅱ、Ⅲ阶段叠加的部位成矿最好.505脉受一近东西向脆-韧性剪切带控制.矿体主要产于断裂的85~90°走向段和倾角为小于45~50°的缓倾段.这些部位也是多次矿化叠加、矿体厚度大、矿石品位高的部位,这些地段也是工业矿体产出的地段.
enyu gold deposit in Henan Province is a large scale auriferous quartz type goldlead deoposit,of which Vein No.505 is the major mined lodeThe spatial occurence of the vein is strictly controlled by an EW stricking brittleductile shear beltThe mineralization process can be divided into 4 stages, which are:(Ⅰ)pyritequartz stage,(Ⅱ)quartzpyrite stage,(Ⅲ)quartzpolymetallic sulfide stage and (Ⅳ)quartzcarbonate stageThe thickness of ore body and grade ofore are controlled by the distribution of auriferous quartz and the superimposed development of the main mineralization stages of Ⅱand ⅢcollectivelyThe structure controlling on gold mineralization shows as follow:1)Affected by the attitude and moving way of orecontrolling fault,the auriferous quartz body mainly occures at the positions where the strike of the fault is less than 90° and the dip angle is less than 50°.2)TheⅡand Ⅲ mineralization stages mainly superimpose at the positions where the strike of the fault is 85~90° and the dip angle is 45~50°.3)The prominent zones by shape of the lying wall of the orecontrolling fault are the positions where the ore shoots locateAnd 4)controlled by the extent of the prominent zones of the lying wall of the orecontrolling fault,the ore shoots in Vein No505 incline west in space
关键词
金矿床
矿化
地质构造
控矿规律
mineralization feature mineralization stage orecontrolling by fault Vein No505 Wenyu gold deposit Henan Province