| 氟镁石-萤石型金矿的成岩成矿机制新探索 |
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| 引用本文： | 郑大中,郑若锋.氟镁石-萤石型金矿的成岩成矿机制新探索[J].江西地质,1999,13(4):288-294. |
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| 作者姓名： | 郑大中 郑若锋 |
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| 作者单位： | 成都综合岩矿测试中心,四川,成都,610081 |
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| 摘 要： | 在岩浆及热液中，氟以氟化硅，硅氟酸迁移，金呈金氢化物，金合金氢化物迁移（或），金，银，铜，铁，铬羰基化合物迁移。在合适的条件下形成氟镁石－萤石型金矿床。
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| 关 键 词： | 氟化硅 硅氟酸 金氢化物 金合金氢化物 金、银、铜、铁、铬羰基化合物 氟镁石-萤石型金矿床 成岩成矿机制 |
AN INVESTIGATION INTO THE ROCK-AND ORE- FORMING MECHANISM OF A SELLAITE-FLUORITE TYPE GOLD DEPOSIT |
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| ZHENG Da-zhong,ZHENG Ruo-feng.AN INVESTIGATION INTO THE ROCK-AND ORE- FORMING MECHANISM OF A SELLAITE-FLUORITE TYPE GOLD DEPOSIT[J].Jiangxi Geology,1999,13(4):288-294. |
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| Authors: | ZHENG Da-zhong ZHENG Ruo-feng |
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| Abstract: | In magma and hydrothermal solution,fluorine is transported in the form of silicon fluoride and silicofluoric acid,gold in the form of gold hydride,gold alloy hydride and/or Au,Ag,Cu,Fe,Cr carbonyl compounds.Under favorable conditions,sellaite-fluorite type gold deposit will be formed from the solution. |
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| Keywords: | silicon fluoride silicofluoric acid gold hydride gold alloy hydride Au Ag Cu Fe Cr carbonyl compounds sellaite-fluorite type gold deposit rock-and ore-forming mechanism |
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