Comparison of sand-layer geometry on flat floors of 10 modern depositional basins
- Duke Univ., Durham, NC
A comparative study of 10 deep turbidite basins indicates that sand-layer thickness, frequency, and continuity can be related to their basin geometries, tectonics, and source areas. This study is based on piston-core data from the flat floors of four oceanic-crust abyssal plains (Sohm, Hatteras, Blake-Bahama, and Silver), two Bahama-Plateau reentrant basins (Columbus basin and Tongue of the Ocean), three subduction zone-island arc basins (Hispaniola-Caicos, Navidad, and St. Croix basins), and one continental-borderland basin (Santa Monica basin). With increasing tectonic activity, sand layers on flat basin floors tend to be thinner and more frequent. Except in elongated narrow basins such as Navidad, source-area size is directly related to proximal sand-layer thickness. Continuity of individual sand layers is a function of drainage-basin size and depositional-basin shape. For example, on the Hatteras Abyssal Plan long-distance continuity (up to 500 km) of individual sand layers is achieved because most of the turbidites are large and are introduced only at the north upstream end. In the small horseshoe-shaped Columbus basin, sand-layer continuity is limited because flows are small and are introduced from three sides. In most basins, sands thin and the percentage of sand layers in the sediment column decreases away from source areas. However, in basins that are small relative to the typical turbidity-current size (e.g., Hispaniola-Caicos basin), the differences between basin-edge and basin-center sand layers are slight. 10 figures, 3 tables.
- OSTI ID:
- 6772631
- Journal Information:
- Am. Assoc. Pet. Geol. Bull.; (United States), Vol. 64:6
- Country of Publication:
- United States
- Language:
- English
Similar Records
Geophysics and structure of Carolina Trough, Blake Plateau, and Bahama Platform
Glacial-interglacial sedimentation rates and turbidite frequency in the Bahamas: a clear case of carbonate shedding during high sea level stands
Related Subjects
02 PETROLEUM
PETROLEUM DEPOSITS
EXPLORATION
SAND
GEOMETRY
SEAS
FLOORS
COMPARATIVE EVALUATIONS
CONTINENTAL MARGIN
DATA
DEPOSITION
DRILL CORES
GEOLOGIC DEPOSITS
TURBIDITY
INFORMATION
MATHEMATICS
MINERAL RESOURCES
RESOURCES
SURFACE WATERS
580100* - Geology & Hydrology- (-1989)
020200 - Petroleum- Reserves
Geology
& Exploration