1965
DOI: 10.1016/0040-1951(65)90038-7
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The evolution of the atlantic mega-undation

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Cited by 27 publications
(4 citation statements)
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“…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.…”
Section: The Present Structural F'eatures Of the Earthmentioning
confidence: 99%
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“…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.…”
Section: The Present Structural F'eatures Of the Earthmentioning
confidence: 99%
“…In the preceding papers on mega-undations (Van Bemmelen, 1964b) the author came to the conclusion, based largely on geotectonic evidence, that the Atlantic and the Indian Ocean Mega-Undations both started in PermoTriassic time, in an area situated somewhere southeast of South Africa (see Fig.6). The &-and q-centres were situated in the neighbourhood of Wegener's South Pole for Late Carboniferous time.…”
Section: The Alpine Cycle Of Orogenymentioning
confidence: 99%
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