摘要
石柱子花岗闪长岩体形成于晚侏罗－早白垩世，岩石属钙碱系列，形成于造山带或岛弧构造环境。岩体的副矿物组合及矿物组合标型研究表明，锆石－磷灰石－锐钛矿（金红石）．锆石－锐钛矿（金红石）．锆石－磷灰石－榍石－金红石（锐钛矿）等３种副矿物组合类型；黄铁矿－黄铜矿－斑铜矿（黝铜矿）－重晶石，黄铁矿－黄铜矿，黄铜矿－方铅矿－重晶石，黄铁矿－黄铜矿－重晶石，黄铁矿－黄铜矿－辉钼矿，黄铁矿－白钨矿，黄铁矿－重晶石等７种矿石矿物组合类型，可作为本区寻找斑岩铜矿的矿物组合标志。
In the Late Jurassic -Early Cretacous,the granodiorite body in Shizhuzi, Kuandian coun-ty,being of calc-alkaline series,formed in an environment of orogenic belt or island arc,Studies on the characterisics of the mineral assemblages show that 3 kinds of accessory min-eral assemblages:zircon- apatite-anatase (rutille),zircon-anatase(rutile),zircon-apatite-ru-tile(anatase),and 7 kinds of ore mineral assemblages:pyrite-chalcopyrite-bronite(te-trahedrite )-barite,pyrite-chalcopyrite,chalcopyrite-galena-barite,pyrite-chalcopyritemolybdenite,pyrite-scheelite,pyrite-barite can be used as the criteria for copper depositprospecting.
出处
《辽宁地质》
1995年第4期272-283,共12页
关键词
铜矿床
找矿标志
花岗闪长岩体
矿物组合
Shizhuzi Kuandian Granodiorite Accessory assemblage Ore mineralassemblage Porphyry copper deposit
