| 老柞山金矿田东部段矿床成因探讨 |
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| 引用本文： | 何宝林.老柞山金矿田东部段矿床成因探讨[J].黄金,2002,23(9):7-12. |
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| 作者姓名： | 何宝林 |
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| 作者单位： | 黑龙江省有色金属地质勘查七○一队 |
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| 摘 要： | 东矿带东部段为老柞山金矿田内最大的金矿床。通过对矿床地质特征的分析，从控矿因素入手，进而阐述矿床演化过程，并指出，老柞山式金矿床的成因类型为再生岩浆热液迭加的混合岩化热液型。
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| 关 键 词： | 矿床地质特征 控矿因素 矿床成因 老柞山式金矿床 |
| 文章编号： | 1001-1277(2002)09-0007-05 |
Discussion on the origion of gold ore deposit at the eastern section of Laozuoshan gold ore field |
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| He Baolin.Discussion on the origion of gold ore deposit at the eastern section of Laozuoshan gold ore field[J].Gold,2002,23(9):7-12. |
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| Authors: | He Baolin |
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| Abstract: | The eastern section gold ore deposit is the biggest one of Laozuoshan gold ore field.Based on the research on geological features of ore deposit and mineralization controlling factores,the paper interprets evolution provess of the ore deposit,and indicates that Laozuoshan gold ore field is formed by compoosite lava which is folded with regeneration lava. |
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| Keywords: | geological feature of ore deposit mineralization controlling factor origion of ore deposit Laozuoshan gold ore field |
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