| 排山楼金矿床的蚀变特征 |
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| 引用本文： | 曲亚军,高殿生,贾云伟,刘贵,白明山,郭宝军,许云鹏.排山楼金矿床的蚀变特征[J].国土资源,1992(1). |
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| 作者姓名： | 曲亚军 高殿生 贾云伟 刘贵 白明山 郭宝军 许云鹏 |
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| 作者单位： | 辽宁省地质矿产局，辽宁省地质矿产局第四地质大队，辽宁省地质矿产局第四地质大队，辽宁省地质矿产局第四地质大队，辽宁省地质矿产局第四地质大队，辽宁省地质矿产局第四地质大队，辽宁省地质矿产局第四地质大队 沈阳 110032，阜新 123000，阜新 123000，阜新 123000，阜新 123000，阜新 123000，阜新 123000 |
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| 摘 要： | 排山楼金矿发育有带状的蚀变晕。蚀变晕明显受韧性剪切带强带控制,从边部向中心根据蚀变强度不同可划分为:绿泥石化带,铁白云石化带和黄铁矿-绢云母化带。金矿化的程度与蚀变强弱关系密切,蚀变愈强金的品位愈高,因此,蚀变晕是寻找金矿的重要标志。
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| 关 键 词： | 辽西 排山楼 金矿 蚀变特征 |
ALTERATION CHARACTERISTICS OF PAISHANLOU GOLD DEPOSIT, WEST LIAONING |
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| Qu Yajun.ALTERATION CHARACTERISTICS OF PAISHANLOU GOLD DEPOSIT, WEST LIAONING[J].Land & Resources,1992(1). |
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| Authors: | Qu Yajun |
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| Abstract: | There are developed altercd halo zones obviously controlled by a strong zone of the ductile shear zone in Paishanlou gold deposit.lt can be divided into three altered zones from outside to inside,according to the strength of the alteration: planar chloritization, ferrodolomitization and pyrite-sericitization zones.The degree of the gold mineralization intergrowing with altered wallrocks are closely concerned with the intensity of alteration, the stronger alteration, the higher the tenor.So the altered halo is the most direct and favorable sign to search for gold deposits. |
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| Keywords: | West Liaoning Paishanlou gold deposit Alteration characteristic |
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