| 云南宾川白象厂构造斑岩蚀变型金矿地质 |
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| 引用本文： | 杨枝斌.云南宾川白象厂构造斑岩蚀变型金矿地质[J].云南地质,2008,27(3):315-319. |
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| 作者姓名： | 杨枝斌 |
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| 作者单位： | 云南省有色地质三一○队,大理,671000 |
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| 基金项目： | 致谢：本文在写作过程中得到三一○队总工程师孙德瑜高工的指导,在此表示衷心感谢. |
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| 摘 要： | 金矿赋存于二长斑岩与玄武岩接触带，局部赋存于二长斑岩与大理岩、玄武岩与大理岩的接触带。脉状、似层状、透镜状产出。矿化受构造及岩体联合控制，为构造斑岩蚀变型金矿床。
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| 关 键 词： | 岩浆岩构造控矿 石英二长斑岩 褐铁矿化 氧化次生淋滤 宾川 白象厂 云南 |
THE GEOLOGY OF BAIXIANGCHANG AU DEPOSIT OF STRUCTURAL PORPHYRY ALTERATION TYPE IN BINCHUAN, YUNNAN |
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| YANG Zhi-bin.THE GEOLOGY OF BAIXIANGCHANG AU DEPOSIT OF STRUCTURAL PORPHYRY ALTERATION TYPE IN BINCHUAN, YUNNAN[J].Yunnan Geology,2008,27(3):315-319. |
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| Authors: | YANG Zhi-bin |
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| Institution: | YANG Zhi-bin (Nonferrous Geological Team 310 of Yunnan ) |
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| Abstract: | The Au deposit exists in the contact between monzonite porphyry and basalt, locally in the contact between monzonite porphyry and marble, basalt and marble. Ore bodies are vein, stratoid or lenticular. The metallogenesis is controlled by the structure and rock body. The ore deposit belongs to the Au deposit of structure porphyry alteration type. |
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| Keywords: | Ore Control of Magmatite and Structure Quartz Monzonite Porphyry Limonitization Oxidized Leached Secondary Deposit Baixiangchang Binchuan Yunnan |
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