Abstract
The purpose of the Gulf Coast Onshore Offshore Experiment, which was carried out in cooperation with the United States Coast and Geodetic Survey, was to determine crustal structure of a section across the Gulf Coast Geosyncline where the sediments are near maximum thickness. There is a longstanding difficulty in conceiving of a mechanism by which the deep sedimentary basins are formed. There appear to be two possibilities: (1) deposition of sediments on a continental crust which was downbuckled to accommodate them by some unknown means; or (2) that wherever the sediments were formed initially, they were finally deposited in deep water. In the latter case one would expect that they would be underlain by a thin oceanic crust.
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