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内蒙古敖脑达坝斑岩型铜银锡多金属矿床围岩蚀变特征研究
引用本文:赵元芝,程泽君.内蒙古敖脑达坝斑岩型铜银锡多金属矿床围岩蚀变特征研究[J].吉林地质,1994,13(2):57-62.
作者姓名:赵元芝  程泽君
作者单位:长春地质学院,内蒙古地矿局115地质队
摘    要:在给出明确的命名原则基础上,将矿床的蚀变围岩划分为五类:黄玉石英交代岩、绿泥石石英交代岩、绢云母石英交代岩、电气石绿泥石化花岗斑岩、钾长石化花岗斑岩。在平面上岩体中心部位为黄玉石英蚀变带,其两侧为绿泥石石英蚀变带;在剖面上由上向下依次出现绿泥石石英蚀变带→黄玉石英蚀变带→绢英岩化带→钾化带→(电气石)绿泥石化带。从蚀变岩石地球化学角度阐述了铜银锡各自不同的成矿部位。

关 键 词:      多金属矿床  围岩蚀变

CHARACTERISTICS OF WALL ROCK AL TERATION OF PORPHYRY TYPE COPPER,SILVER AND TIN POLYMETAL DEPOSIT,AONAODABA ,INNER MONGOLIA
Zhao Yuanyi Li Dianchao.CHARACTERISTICS OF WALL ROCK AL TERATION OF PORPHYRY TYPE COPPER,SILVER AND TIN POLYMETAL DEPOSIT,AONAODABA ,INNER MONGOLIA[J].Jilin Geology,1994,13(2):57-62.
Authors:Zhao Yuanyi Li Dianchao
Abstract:n the basis of giving nomenclature,the altered rocks of this deposit can be divided into five types:topaz-quartz metasomatite,chlorite-quartz metasomatite,sericite-quartzmetasomatite,tourmaline-chloritization granite-porphyry and potassifeldspar granite- porphyry.Horizontally,the topaz-quartz alteration zone is located in the central part,andthe chloritequartz alteration zone is on the both sides of it.In the vertical zone,from the up-per to below,there are following alteration zones:chloritequartz-topazquartz-sericitization- potassic-(tourmaline)chlorite.By means of geochemistry,this paper describes the differ-ent ore- forming postions of copper,silver and tin.
Keywords:metasomatic rock Hornfels Thermal electromotive force valueAonaodaba  
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