【摘要】 凹地苴铜矿矿物在剖面上具从辉铜矿－ 斑铜矿－ 黄铜矿－ 黄铁矿分带现象。几个分带相互叠加，矿床形成于氧化还原界面附近。种种证据表明含矿溶液因多阶段脱水形成，矿床是通过双层卤水在氧化还原界面附近相互反应成矿更多还原

【Abstract】 Metal minerals in Wadizhou copper deposit appear to be zoning of chalcosine bornite chalcopy rite pyrite on the vertical direction. The mineral zones are Lapped each other, and the ore deposit is located near the interface of reduction oxidation. A great deal of evidences have shown that the deposit was formed at the result of reaction of two layers brine water, which was from multi stage dewatering.更多还原