Problems concerning the evolution of oceanic lithosphere in the northern Red Sea
The pole of rotation for the opening of the Red Sea at 36.5°N, 18.0°E (Arabia from Africa) implies the fastest spreading rates are in the south and are about 50% less in the north. Various studies show the spreading rate in the south to be about 1 cm/yr over the last 4–5 Ma. Problems arise as to the...
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Veröffentlicht in: | Tectonophysics 1985-01, Vol.116 (1), p.109-122 |
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Format: | Artikel |
Sprache: | eng |
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