Shallow Structure of the Straits of Florida

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Science  29 Jul 1966:
Vol. 153, Issue 3735, pp. 529-531
DOI: 10.1126/science.153.3735.529


Continuous seismic profiles of the Straits of Florida indicate that north of 26°30'N the trough was formed mainly by sediment upbuilding along the margins. South of this latitude the straits may be due in part to faulting.