| 会理县小青山铜金矿区硅质钠长石岩研究 |
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| 引用本文： | 靳西祥.会理县小青山铜金矿区硅质钠长石岩研究[J].矿物岩石,1992,12(4):48-56. |
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| 作者姓名： | 靳西祥 |
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| 作者单位： | 宜昌地质矿产研究所 宜昌 |
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| 摘 要： | 岩石空间产出特征、岩相学、岩石化学、稀土元素地球化学特征及成岩成矿作用特征等分析研究表明,硅质钠长石岩是经沉积变质、硅质钠质交代作用形成的,原岩组成多样,主要为碳质板岩,其次为条带状泥砂质白云岩,局部也可以是辉绿辉长岩。
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| 关 键 词： | 铜矿床 金矿床 钠长石 硅质 岩岩 |
STUDY OF THE SILICEOUS ALBITE ROCK IN XIAOQING SHAN Cu-Au ORE DISTRICT,HUILI COUNTY SICHUAN |
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| Jin Xixiang.STUDY OF THE SILICEOUS ALBITE ROCK IN XIAOQING SHAN Cu-Au ORE DISTRICT,HUILI COUNTY SICHUAN[J].Journal of Mineralogy and Petrology,1992,12(4):48-56. |
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| Authors: | Jin Xixiang |
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| Abstract: | The analysis and study of the spatial occurrence characteristics of the siliceous albite rock, petrofabrics, petrochemistry, REE geochemistry and diagenetic-minerogenetic characteristics indicated that the siliceous albite rock was formed through the sedimentary-metamorphism,siliceous-sodic metasomatism. Their primary rock assemblage is various,and composed mainly of carbonaceous slate,then minor striped mud-sand dolomite,and may be some diabase-gabbro locally. |
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| Keywords: | siliceous albite rock sedimentary-metamorphism siliceous-sodic metasomatism diagenetic-minerogenesis Xiaoqing Shan |
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