| 热液石油与金属成矿流体的形成 |
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| 引用本文： | 付修根.热液石油与金属成矿流体的形成[J].资源调查与环境,2005,26(2):114-119. |
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| 作者姓名： | 付修根 |
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| 作者单位： | 成都理工大学地球科学学院,四川成都,610059 |
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| 摘 要： | 本文介绍了热液石油形成的温度、运移方式几个方面的特征。通过实例证实了热液石油与成矿流体具有共生关系。在热液石油的形成过程中，有机酸、烃类、NSO极性化合物等组分直接参与了成矿物质的活化、迁移作用，而有机质在演化过程中的体积膨胀作用则为成矿物质的带出提供了通道。
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| 关 键 词： | 热液石油 有机酸 成矿流体 |
| 文章编号： | 1671-4814(2005)02-114-06 |
| 修稿时间： | 2004年11月2日 |
Hydrothermal petroleum and metal minerogenic fluid formation |
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| FU Xiu-gen.Hydrothermal petroleum and metal minerogenic fluid formation[J].Resources Survey & Environment,2005,26(2):114-119. |
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| Authors: | FU Xiu-gen |
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| Abstract: | The paper briefly introduces the forming temperature and migration of hydrothermal petroleum in order to prove there exists paragenetic relationship between hydrothermal petroleum and ore-forming fluids by some evidence examples. During the formation of hydrothermal petroleum, organic acids, hydrocarbon compounds and NSO-polar compounds et al are involved in the activation and migration of ore-forming process. Volume of expansion of organic material during the evolution provides a pathway for the ore-forming fluids to flow out easily. |
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| Keywords: | hydrothermal petroleum organic acid ore-forming fluid |
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