| 海洋和大陆岩石圈下的混合地幔对流模型 |
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| 引用本文： | 张健,石耀霖.海洋和大陆岩石圈下的混合地幔对流模型[J].中国科学院研究生院学报,1998(2). |
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| 作者姓名： | 张健 石耀霖 |
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| 作者单位： | Graduate School，Academia Sinica，Beijing 100039 |
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| 摘 要： | 运用参量化模型方法，建立了海洋岩石圈板块和大陆岩石圈板块下混合地幔对流模型．计算结果表明：板块构造和地幔对流的相互作用，造成在地球演化的晚期海洋岩石圈板块和大陆岩石圈板块下的地幔幕式翻转不同步，导致海洋板块和大陆板块之间的边缘地带成为构造活跃地区．
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| 关 键 词： | 海洋板块，大陆板块，混合地幔对流，参量化模型 |
The Parameterized Mixed Mantle Convection Models of Continent and Ocean |
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| Zhang Jian\ Shi Yaolin.The Parameterized Mixed Mantle Convection Models of Continent and Ocean[J].Journal of the Graduate School of the Chinese Academy of Sciences,1998(2). |
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| Authors: | Zhang Jian\ Shi Yaolin |
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| Abstract: | Introduces the parameterized method built the mixed mantle convection models beneath oecanic and continental lithosphere.The result shows that the action between mantle and plate lead in a nonsynchronous of the overturn between oceanic and continental mantle in the later period of earth evolution.This nonsynchronou can cause the tectonic activity in the marginal zone between oceanic and continental lithosphere. |
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| Keywords: | oceanic plate continental plate mixed mantle convection thermal evolution parameterized model |
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