The Early Gulf of Mexico as a Subaerial Basin Below Sea Level (SABSEL) Basin. Evidence from Stratigraphy and Facies of Luanne salt, Norphlet sandstone and Smackover Brown Dense Formations.

Martin M Cassidy, University of Houston, Earth & Atmospheric Sciences, Houston, TX, United States
Back to: Mesozoic to Recent Evolution of the Gulf of Mexico Basin from Integrated Geologic and Geophysical Data Sets I Posters