| 地幔对流模式及其意义 |
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| 引用本文： | 陈阳阳,王大丰,周龙,柳立业,胡宸,于雷,魏海峰.地幔对流模式及其意义[J].世界有色金属,2020(1):202-202,204. |
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| 作者姓名： | 陈阳阳 王大丰 周龙 柳立业 胡宸 于雷 魏海峰 |
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| 作者单位： | 中国地质调查局哈尔滨自然资源综合调查中心;中国人民武装警察部队黄金第三支队 |
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| 基金项目： | 地调项目：东北边境长白-珲春地区综合地质调查 |
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| 摘 要： | 地幔对流是地球深部物质运动的重要形式之一,对板块构造起着重要作用。为解决其机制,地质学家们提出了一系列模式,本文对多种地幔对流模式进行分析论述。但关于地幔对流机理方面的分歧依然存在,主要是:①地幔对流的能量来源②地幔对流的深度。
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| 关 键 词： | 地幔对流 模式 |
Mantle Convection Model and Its Significance |
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| CHEN Yang-yang,WANG Da-feng,ZHOU Long,LIU Li-ye,HU Chen,YU Lei,WEI Hai-feng.Mantle Convection Model and Its Significance[J].World Nonferrous Metals,2020(1):202-202,204. |
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| Authors: | CHEN Yang-yang WANG Da-feng ZHOU Long LIU Li-ye HU Chen YU Lei WEI Hai-feng |
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| Affiliation: | (Harbin Natural Resources Comprehensive Investigation Center,China Geological Survey,Harbin 150000,China;The Third Gold Detachment of the Chinese Armed Police Force,Haerbin 150000,China) |
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| Abstract: | Mantle convection is one of the important forms of deep earth material movement and it plays an important role in plate tectonics.In order to solve the mechanism,many geologists have proposed a series of models.However,there are still controversies on the mechanism of mantle convection,mainly as follows:①the energy source of mantle convection;and②the depth of mantle convection. |
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| Keywords: | mantle convection model |
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