| 赵以辛,吴夫军.辽宁阜新排山楼金矿容矿岩石及其含金性研究[J].地质找矿论丛,1998,(2):56-66 |
| 辽宁阜新排山楼金矿容矿岩石及其含金性研究 |
| STUDY ON THE HOST ROCK AND ITS ORE BEARING CAPACITY OF PAISHANLOU AU DEPOSIT |
| 投稿时间：1998-02-13 修订日期：1998-02-20 |
| DOI：10.6053/j.issn.1001-1412.1998.2. 007 |
| 中文关键词: 容矿岩石类型 微量元素特征 含金性 |
| 英文关键词:host rock types micro element characteristics Au ore bearing capacity |
| 基金项目:地质行业基金 |
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| 中文摘要: |
| 研究结果表明,排山楼金矿的容矿围岩是一套以英云闪长岩为主体,含少量角闪质上壳岩包体及脉岩的组合。这套英云闪长岩加脉岩(闪长玢岩)系经强变形作用改造,形成排山楼金矿现有的含矿糜棱岩系。容矿角闪质糜棱岩中金与钯关系研究结果不支持金矿质直接来自于矿体附近的角闪质上壳岩包体说法。 |
| 英文摘要: |
| Paishanlou large size Au deposit is hosted by tonalite in which upper crustal amphibolitic rock inclusions occur. After strong deformation it is directly hosted by amphibolitic mylonite.Relationship of palladium and gold in the mylonite reveals no evdence to support direct source of Au ore materials from the upper crustal amphibolitic rock inclusions. |
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