| 论深源流体参与黔西南金矿床成矿的可能性 |
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| 引用本文： | 朱赖民,金景福.论深源流体参与黔西南金矿床成矿的可能性[J].地质论评,1997,43(6):586-592. |
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| 作者姓名： | 朱赖民 金景福 |
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| 作者单位： | 中国科学院地球化学研究所，成都理工学院，成都理工学院，中国科学院地球化学研究所，中国科学院地球化学研究所 贵阳，贵阳，贵阳 |
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| 基金项目： | 中国科学院矿床地球化学开放实验室资助项目 |
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| 摘 要： | 通过研究黔西南金矿床时空分布及地球化学特征，讨论了深源流体参与金矿床成矿的可能性。金矿床在时空上受莫面隆起，深大断裂，幔源岩浆岩体的控制，且与航磁异常，重力异常，环形构造等存在对应关系。
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| 关 键 词： | 深源流体 金矿床 矿床成矿 可能性 |
ON THE POSSIBILITY OF THE PARTICIPATION OF JUVENILE FLUIDS IN THE GOLD DEPOSIT FORMATION IN SOUTHWESTERN GUIZHOU |
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| Zhu Laimin.ON THE POSSIBILITY OF THE PARTICIPATION OF JUVENILE FLUIDS IN THE GOLD DEPOSIT FORMATION IN SOUTHWESTERN GUIZHOU[J].Geological Review,1997,43(6):586-592. |
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| Authors: | Zhu Laimin |
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| Abstract: | According to the time and space distribution and geochemistry of gold deposits in southwestern Guizhou, in this paper is discussed the possibility of the participation of juvenile fluids in the gold deposit formation. The gold deposits are constrained by the uplift of the Moho, deep faults and mantle-derived magmatic rock bodies, and correspond in space with deromagnetic anomalies, gravity anomalies and circular structures. The study of lead, sulfur, hydrogen and oxygen isotopes and REE geochemistry indicates that the ore material might come from juvenile fluids and crustal rocks. The gold deposits are the product of reworking of crustal rocks by juvenile fluids. |
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| Keywords: | juvenile fluid gold deposit southwestern Guizhou province |
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