知识与财富的链接
条山铁、铜多金属矿床位于华北板块与扬子板块的接合部位、秦岭多金属成矿带东段桐柏-大别山成矿亚带内,区内构造线呈NWW向展布,含矿地层为二郎坪群变细碧-角斑岩系,它经历了4个喷发旋回,形成了本区多金属成矿的4个含矿层位.第一旋回的顶部为一富铁矿层,为姑山式火山熔浆型含铜锌磁铁矿层;该层位自陕西三条岭,向东经汤河、太坪镇至...
The Tiaoshan iron-copper polymetallic deposit is situated in the conjunction area between the North China plate and Yangtze plate,in the Tongbai-Dabieshan metallogenic sub-belt,eastern section of the Qinling polymetallic mineralization belt.Tectonic lines in this region extend in NWW direction.The ore-bearing stratum is spilite-keratophyre in the Erlangping Group.It has undergone four eruption cycles,forming four ore-bearing horizons in this area.The top of the first cycle is an iron-rich ore layer,belongin...
