The South Florida Basin of the eastern Gulf of Mexico represents a vast, undisturbed carbonate system that extended from the Florida Keys through the Tampa-Sarasota Arch. In South Florida, extensive subsurface data and analogous modern environments provide an opportunity to unravel the evolution of this system from shoreline to shelf-margin. This study examines the changing facies and the pore network of the Latest Aptian-Early Albian Sunniland interval. Stratigraphic results are closely comparable with contemporary carbonate platform studies in the northern Gulf of Mexico. The Sunniland Formation was deposited during a major transgressive-regressive sequence. The Sunniland interval is divided into five third-fourth order, transgress-regr...
High-resolution seismic-reflection data collected along the length of the Caloosahatchee River in so...
Successful hydrocarbon exploration in former rift basins of the South Atlantic pre-salt has generate...
The middle Santonian-lower Campanian carbonate-mud dominated succession deposited in the northeaster...
The South Florida Basin of the eastern Gulf of Mexico represents a vast, undisturbed carbonate syste...
textCarbonate platforms contain a wealth of information regarding the changing biota, sea level, oce...
textThis study examines the regional stratigraphic architecture, depositional systems, and petrograp...
High-resolution seismic-reflection data collected along the length of the Caloosahatchee River in so...
The late Permian Queen Formation (115 m thick) is a succession of mixed clastics, carbonates and eva...
textFor decades the Upper Cretaceous Lower Tuscaloosa Formation of the U.S. Gulf Coast has been cons...
During the early Cretaceous (Valanginian-Hauterivian stages), there were significant basin- to regio...
The Pettet Limestone of the Wright Mountain field on the northeastern flank of the East Texas Basin ...
textHigh-resolution sequence stratigraphy coupled with understanding of diagenetic processes within...
textHigh-resolution sequence stratigraphy coupled with understanding of diagenetic processes within...
The Upper Cretaceous Buda Formation is a highly bioturbated, naturally fractured chalk unit deposite...
The Upper Cretaceous Buda Formation is a highly bioturbated, naturally fractured chalk unit deposite...
High-resolution seismic-reflection data collected along the length of the Caloosahatchee River in so...
Successful hydrocarbon exploration in former rift basins of the South Atlantic pre-salt has generate...
The middle Santonian-lower Campanian carbonate-mud dominated succession deposited in the northeaster...
The South Florida Basin of the eastern Gulf of Mexico represents a vast, undisturbed carbonate syste...
textCarbonate platforms contain a wealth of information regarding the changing biota, sea level, oce...
textThis study examines the regional stratigraphic architecture, depositional systems, and petrograp...
High-resolution seismic-reflection data collected along the length of the Caloosahatchee River in so...
The late Permian Queen Formation (115 m thick) is a succession of mixed clastics, carbonates and eva...
textFor decades the Upper Cretaceous Lower Tuscaloosa Formation of the U.S. Gulf Coast has been cons...
During the early Cretaceous (Valanginian-Hauterivian stages), there were significant basin- to regio...
The Pettet Limestone of the Wright Mountain field on the northeastern flank of the East Texas Basin ...
textHigh-resolution sequence stratigraphy coupled with understanding of diagenetic processes within...
textHigh-resolution sequence stratigraphy coupled with understanding of diagenetic processes within...
The Upper Cretaceous Buda Formation is a highly bioturbated, naturally fractured chalk unit deposite...
The Upper Cretaceous Buda Formation is a highly bioturbated, naturally fractured chalk unit deposite...
High-resolution seismic-reflection data collected along the length of the Caloosahatchee River in so...
Successful hydrocarbon exploration in former rift basins of the South Atlantic pre-salt has generate...
The middle Santonian-lower Campanian carbonate-mud dominated succession deposited in the northeaster...