| 老柞山金矿床地质特征及同位素地球化学特征 |
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| 引用本文： | 张红军. 老柞山金矿床地质特征及同位素地球化学特征[J]. 地质找矿论丛, 1999, 14(1): 48-52,87 |
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| 作者姓名： | 张红军 |
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| 作者单位： | 中国地质大学（武汉）研究生院 |
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| 摘 要： | 通过对赋存于麻山群老地层且与岩浆热液有关的老柞山金矿床的矿床地质及稳定同位素地球化学特征的研究分析，得出老柞山金矿床与岩浆岩、构造和麻山群密切相关，岩浆热液提供物源和热源，区内成矿物质具有深源性且来源单一的特点。
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| 关 键 词： | 金矿床 同位素地球化学 老柞山 地质特征 |
| 收稿时间： | 1999-01-22 |
STUDY ON THE GEOLOGY AND ISOTOPE GEOCHEMISTRY OF LAOZHUOSHAN GOLD DEPOSIT |
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| Zhang Hongjun. STUDY ON THE GEOLOGY AND ISOTOPE GEOCHEMISTRY OF LAOZHUOSHAN GOLD DEPOSIT[J]. Contributions to Geology and Mineral Resources Research, 1999, 14(1): 48-52,87 |
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| Authors: | Zhang Hongjun |
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| Affiliation: | China University of Geoscience, Graduate Scholl, 430074 |
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| Abstract: | Based on the studies of geology and isotope geochemistry of Laozhuoshan gold deposit, we can get important information about the deposit. It is concluded that magmatic hydrothermal fluid provides ore forming material, and ore forming material has the character of deep and single source (derived form upper mantle and lower crust). The deposit is closely related to magmatic thermal fluid, structure and Mashan group (Ptm). This is confirmed by regional geology and the characters of Pb, S, C and O stable isotopes. |
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| Keywords: | Gold deposit isotope goechemistry Laozhuoshan |
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