Abstract
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.
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.
