| 辽南隈子金矿矿床地质特征及其成因探讨 |
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| 引用本文： | 申少华,裴喜.辽南隈子金矿矿床地质特征及其成因探讨[J].国土资源,1994(4). |
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| 作者姓名： | 申少华 裴喜 |
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| 作者单位： | 中国有色金属工业总公司北京矿产地质研究所，中国有色金属工业总公司辽宁地质勘查局地质研究所 |
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| 基金项目： | 国家黄金管理局科研项目 |
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| 摘 要： | 隈子金矿产于似斑状黑云母花岗岩所包围的辽河群盖县组残留体中，矿脉明显受层间断裂控制。矿石特征，硫、氧同位素，包裹体及红外光谱综合研究表明：隈子金矿床属中－高温成矿，成矿流体呈重熔岩浆热液特征。因此，该矿床是重熔岩浆热液矿床。
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| 关 键 词： | 隈子，石英脉，金矿 |
DISCUSSION ON GEOLOGICAL CHARACTER AND GENESIS OF WAIZI GOLD DEPOSIT IN SOUTHERN LIAONING |
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| Shen Shaohua.DISCUSSION ON GEOLOGICAL CHARACTER AND GENESIS OF WAIZI GOLD DEPOSIT IN SOUTHERN LIAONING[J].Land & Resources,1994(4). |
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| Authors: | Shen Shaohua |
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| Abstract: | Waizi gold deposit occurs in remanent Gaixian Formation of Liaohe Group besieged byporphyroid biotite granite. Ore vein is under the control of interformational fault obviously. The research on the geological characters of ore, inclusion, sulfur and oxygen isotope, in-frared spectrum shows that Waizi deposit belongs to meso-high temperature mineralization.The ore fluid behaves the features of remelting magmatic hydrothermal solution. Thus, Waizideposit is a remelting magmatic hydrothermal deposit. |
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| Keywords: | Waizi Quartz vein Gold deposit |
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