| Mantle plume generates at the junction of parts of the core-mantle magma equivalent of a "magma ocean", the lower mantle and upper mantle, upper mantle and the asthenosphere magma flow of Road between the equivalent of a "river of magma," magma from the asthenosphere through the lithosphere spray out of the ground in between the channels, the equivalent of "magma stream." Between them, there will be many "magma tributary", which the "tributary" to these "river" and "river" or "river" and "stream" between linked. Sub-sub-oceanic mantle plume is due to the existence of horizontal "magma tributary", which lateral flow, generated in the rock at the bottom of the shear stress in the opposite direction, making ocean crust and oceanic crust created between the displacement of dislocation. A sub-oceanic ridge "magma tributary" in depth, size, produced by stress have to be much larger than two, three, four. This and previous studies mainly affected by sub-ridge mantle upwelling of magma pulse control of non-cyclical dynamics are essentially different in nature. |
