| 岩石圈不连续与大陆成矿作用 |
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| 引用本文：.2004.Lithospheric Discontinuity and Continental Metallogenesis[J].Mineral Deposits,23(Z):32~40 |
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| 基金项目:中国地质调查局项目（K1.4-1-2和200113900018）、国家自然科学基金重点项目（NSFC 402344048）、国土资源部科技专项计划项目（20001010202和200010103）、“中国三维岩石圈深部物质模型研究”课题、中国科技部IGCP国际合作项目（2001cb711002）和中国地质大学“岩石圈构造、深部过程及探测技术”教育部重点实验室开放课题（2003009和2003010） |
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| 中文摘要:岩石圈不连续是岩石圈块体间的构造薄弱带，也是岩石圈单元和深部成矿单元划分的重要界线；本文以华北地台为例，阐述岩石圈不连续的概念，初步探讨了岩石圈不连续在大陆成矿作用过程中的作用，并讨论了岩石圈不连续的识别标志。 |
| 中文关键词:岩石圈不连续 大陆成矿作用 识别标志 |
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| Lithospheric Discontinuity and Continental Metallogenesis |
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| Abstract:Lithospheric discontinuities are tectonic weak belts between the lithospheric blocks, and also serve as important borderlines for the division of lithospheric units and deep metallogenic units. This paper has expounded the concept of lithospheric discontinuities with North China platform as an example, probed into the roles of the lithospheric discontinuities in the process of continental metallogenesis, and discussed the identifying criteria of lithospheric discontinuities. |
| keywords:lithospheric discontinuity, continental metallogenesis, identifying criteria |
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