“…This type of oceanization is the result of "penetrative convection", of the upper mantle, as defined by MacDonald (1965, p.225); whereas the Atlantic type of oceanization might be interpreted as gravity flow of the outer layers due to "mega-convection" in the entire mantle. The mechanism of this mega-convection might more or less conform to the ideas put forward by Bernal (1961), Orowan (1965), and Van Bemmelen (1964b. A major riddle still is the origin of the Pacific Ocean.…”