| 部分熔融与青藏高原地壳加厚的关系综述 |
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| 引用本文： | 杨晓松,金振民.部分熔融与青藏高原地壳加厚的关系综述[J].地质科技情报,1999(1):14. |
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| 作者姓名： | 杨晓松 金振民 |
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| 作者单位： | 中国地质大学地球科学学院,武汉,430074 |
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| 基金项目： | 国家自然科学基金,地矿部行业基金,博士点基金 |
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| 摘 要： | 从地球物理学、实验岩石学、岩石学和地球化学几个方面论述了青藏高原已具备壳内发生大规模部分熔融的物理环境及物质基础；并讨论了壳内部分熔融与青藏高原地壳加厚的关系和三种可能的加厚方式
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| 关 键 词： | 部分熔融作用 底侵作用 巨厚地壳 青藏高原 |
| 修稿时间： | 1998-09-03 |
RELATIONSHIP BETWEEN INTRACRUSTAL PARTIAL MEL-TING AND THICKENING OF TIBETAN PLATEAU CRUST |
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| Yang Xiaosong,Jin Zhenming.RELATIONSHIP BETWEEN INTRACRUSTAL PARTIAL MEL-TING AND THICKENING OF TIBETAN PLATEAU CRUST[J].Geological Science and Technology Information,1999(1):14. |
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| Authors: | Yang Xiaosong Jin Zhenming |
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| Abstract: | From several aspects,such as geophysics,experimental petrology,petrology and geochemistry,this paper states that there are physical conditions and material basis of melting in wide scale in Tibetan Plateau.Then the relationship between intracrustal partial melting and thickening of Tibetan Plateau as well as three possible thickening models are discussed. |
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| Keywords: | partial melting underplating anomalously thickening crust Tibetan Plateau |
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