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Petrology and mineral chemistry of sedimentary rocks from the Western Solomon Sea
Authors:Keith A W Crook
Institution:(1) Woods Hole Oceanographic Institution, 02543 Woods Hole, MA
Abstract:Multichannel seismic reflection profiles recorded in the northern Red Sea show structures that we interpret to be a result of the intrusion of uppermost Miocene salt. We believe that the evaporites are underlaid by attenuated continental crust and the flow of salt is due to renewed faulting of basement in the Pliocene when sea floor spreading began between latitudes 21°N and 15°30°N.
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