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Plate tectonics and mantle controls on plume dynamics

机译:羽流动力学板构造和地幔控制

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摘要

Mantle plumes provide valuable information about whole-mantle convection: they originate at the coremantle boundary, cross Earth's mantle and interact with the lithosphere. For instance, it has been proposed that the mobility/stability of plumes depends on plume intrinsic properties, on how slabs interact with the basal boundary layer, on mantle flow, or on their proximity to mid-ocean ridges.
机译:Mantle Plumes提供有关全套地幔对流的宝贵信息:它们起源于Coremantle边界,越过地球的地幔并与岩石圈进行互动。 例如,已经提出了羽毛的迁移率/稳定性取决于羽流内在特性,在平板上与基底边界层相互作用,在地幔流动上或其接近中海脊上。

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