| 香炉碗子金矿床稳定同位素研究及矿床成因探讨 |
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| 引用本文： | 李长顺,于文卿.香炉碗子金矿床稳定同位素研究及矿床成因探讨[J].黄金地质,1996,2(2):50-55. |
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| 作者姓名： | 李长顺 于文卿 |
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| 作者单位： | 核工业东北地勘局２４４大队 |
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| 摘 要： | 香炉碗子金矿床产于脆一韧性剪切带内，控矿围岩为火山隐爆角砾岩体，通过硫，铅，氢，氧，碳，锶等同位素及稀土元素的研究可以看出，该矿床是一个中，低温有大气水参与火山热液型金矿床，其火山岩岩浆属太古宙结晶基底重熔再造，壳幔混合型。
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| 关 键 词： | 金矿床 稳定同位素 矿床成因论 |
STUDY ON STABLE ISOTOPE AND ORE GENESIS OF XIANGLUWANZI GOLD DEPOSIT |
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| LiChangshunYuWenqing.STUDY ON STABLE ISOTOPE AND ORE GENESIS OF XIANGLUWANZI GOLD DEPOSIT[J].Gold Geology,1996,2(2):50-55. |
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| Authors: | LiChangshunYuWenqing |
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| Abstract: | Xiangluwanzi gold deposit occurs in the brittleductile shear zone. The volcanic crytoexplosive breccia body is orecontrolling wall rock. The analysis of H,O,C and Sr isotopes shows that this deposit is a lowtomoderate temperature volcanogene hydrothermal gold deposit in which meteoric water participates. The magma belongs to the crustmantle mixed type of Archeozoic crystalline basement remelted and recomposed. |
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| Keywords: | gold deposit volcanic crytoexplosive breccia body stable isotope ore genesis Jilin |
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