| 排山楼金矿地质特征及成矿模式初探 |
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| 引用本文： | 李达,韩雪梅.排山楼金矿地质特征及成矿模式初探[J].地质与资源,1995,4(2):109-117. |
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| 作者姓名： | 李达 韩雪梅 |
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| 作者单位： | 辽宁省地质矿产局第四地质大队 |
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| 摘 要： | 排山楼金矿赋存于排山楼一侯其营子韧性剪切带内,发育有与金矿有密切成生联系的围岩蚀变带。金矿物在矿石内以晶隙金、裂隙金为主。极少量的包裹金。从矿液的形成至矿体的定位,经历了两个发展阶段,即早期的韧性变形阶段和晚期的脆一韧性变形阶段。
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| 关 键 词： | 排山楼 金矿 地质特征 成矿模式 |
GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF GOLD DEPOSITS AT PAISHANLOU |
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| Li Da,Hanxuemei.GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF GOLD DEPOSITS AT PAISHANLOU[J].Geology and Resources,1995,4(2):109-117. |
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| Authors: | Li Da Hanxuemei |
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| Institution: | The Fourth Geological Team, Liaoning Bureau of Geology and Mineral Resources. Fuxin 123000 |
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| Abstract: | Paishanlou gold deposits occurred in Paishanlou-Houqiyingzhi ductile shear zone, There aredeveloped altered halo zones that is closely concerned with the degree of the gold mineralization. |
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| Keywords: | Paishanlou gold deposit geological characteristics metallogenic model |
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