![]() ![]() Mantle convection and their possible dynamics within the concept of geosynclinal tectonics. ![]() East-west- and south-west oriented flows of The eastern branch is most likely the flow of mantle convection from the core to the earth's crust (Fig. ![]() west- and southwest-orientedįlows of mantle convection. Deformation events in the CRH suggest east. sequentially restore three cross sections.
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