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Regularities of Spatial Distribution of Mantle Hot Spots of the Modern Earth

机译:现代地球地幔热点的空间分布规律

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摘要

The mantle hot spots of the modern Earth were first found by P. Morgan and G. Wilson as projections of the deep-earth material flows at the modern Earth's surface, uplifting under the moving lithosphertc plates [1,2]. Since that time, the study of interplate oceanic and continental magmatism and geodynamics associated with the mantle hot spots has advanced the development of this hypothesis. It has led to development of the patterns of their deep structure [3] on the one side, and, actually, negation of their deep structure, on the other side [4]. The most prominent achievement of modern geophysics and geology is the development of visual images of the mantle plumes on the basis of global and local seismic tomography. A recent review of such works is presented in [5]. The given work is devoted to discussion of a poorly studied problem, the estimation of regularities of the spatial distribution of the hot spots in the Earth and their connection with modern and ancient geodynamic processes.
机译:P. Morgan和G. Wilson首先发现了现代地球的地幔热点,原因是深地球物质在现代地球表面流动的投影,在移动的岩石圈板下隆起[1,2]。从那时起,与地幔热点相关的板间海洋和大陆岩浆作用和地球动力学的研究推动了这一假说的发展。它一方面导致了其深层结构模式的发展[3],另一方面却导致了对它们深层结构的否定[4]。现代地球物理学和地质学最突出的成就是在全球和局部地震层析成像技术的基础上发展了地幔柱的可视图像。在[5]中介绍了对此类作品的最新评论。所提供的工作致力于讨论一个尚未深入研究的问题,估算地球上热点的空间分布的规律性及其与现代和古代地球动力学过程的联系。

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  • 来源
    《Doklady Earth Sciences》 |2009年第6期|924-928|共5页
  • 作者单位

    Institute of Ore Deposits, Geology, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, ul. Bol'shaya Gruzinskaya 10, Moscow, 123995 Russia;

    Institute of Ore Deposits, Geology, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, ul. Bol'shaya Gruzinskaya 10, Moscow, 123995 Russia;

    Institute of Ore Deposits, Geology, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, ul. Bol'shaya Gruzinskaya 10, Moscow, 123995 Russia;

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