Convection currents is a fairly accepted idea as far as the deriving mechanism of plate tectonics is concerned, what are the latest developments about the deriving mechanism?
Recent studies showing the decoupling of the lithosphere from the underlying asthenosphere hints that other, equally important, driving forces for plate tectonics are required. A very useful paper on this discussion is Riguzzi et al. 2009, tectonophysics.
Any lubricant can provide the conditions for movement. But for the most distant horizontal motion of the plates (even if lubricated) very powerful forces are needed. Perhaps the spreading of plumes can cause collisions, obduction, subduction (limited by the same spatial framework as the collision).
I do not know anything about global hydrothermal flows. Do you mean asthenosphere?
Gentlemens, it seems to me that we are looking for a mechanism for a phenomenon that has not yet been fully proved? The kinematics of the long-distance movement of plates do not get caught up globally. Perhaps it is more rational to retreat back to the time of the birth of platectonics and to assess its compliance with new facts about the structure of the crust and mantle?