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- W2010705439 abstract "Based on the high resolution body wave tomographic images and relevant geophysical data we calculated the form and vertical velocity of mantle flow, and obtained the global vertical moving pattern of mantle flow. On a globe scale the mantle flow can be divided into several regions, the two large-scale mantle downwelling regions in Eurasian-Australian continents and North American-South American continents, and two large-scale mantle upwelling regions in the mid and south Pacific Ocean and west Indian Ocean-African-Atlantic Ocean, The mantle upwelling is originated from the core-mantle boundary and mostly presents in the middle mantle and lower part of the upper mantle. The velocity of vertical mantle flow is about 1 to 4 cm per year. The mantle flow controls plate motions and the distributions of ocean ridges, subduction zones and collision zones. The mantle upwelling regions are clearly related with locations of hot-spots on the earth's surface. There is an upwelling plume beneath East Asia and western Pacific which is earth's deep origin for huge rifts. Siberian clod downwelling dives from the surface to near CMB. The tethyan diving region centred in the Qinghai-Tibet Plateau is visible. The three regions of mantle convection beneath East Asia and western Pacific agree with tectonic features of western Pacific, Asia and tethyan regions." @default.
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- W2010705439 date "2006-07-01" @default.
- W2010705439 modified "2023-10-14" @default.
- W2010705439 title "A Study of Global Vertical Velocity of Mantle Flow" @default.
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- W2010705439 doi "https://doi.org/10.1002/cjg2.911" @default.
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