Shallow Structure of the Straits of Florida
- 29 July 1966
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 153 (3735) , 529-531
- https://doi.org/10.1126/science.153.3735.529
Abstract
Continuous seismic profiles of the Straits of Florida indicate that north of 26 degrees 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.Keywords
This publication has 2 references indexed in Scilit:
- Continuous Seismic Profiles of the Continental Terrace off Southeast FloridaGSA Bulletin, 1966
- Bathymetry and geology of Pourtales Terrace, FloridaMarine Geology, 1964