Skip Nav Destination
Close Modal
Update search
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
Filter
- Title
- Author
- Author Affiliations
- Full Text
- Abstract
- Keyword
- DOI
- ISBN
- EISBN
- ISSN
- EISSN
- Issue
- Volume
- References
- Paper Number
NARROW
Format
Subjects
Article Type
Date
Availability
1-9 of 9
Keywords: seaward
Close
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
Sort by
Proceedings Papers
Geological and Shallow Salt Tectonic Setting of the Mad Dog and Atlantis Fields: Relationship Between Salt, Faults, and Seafloor Geomorphology
Available to PurchaseDaniel L. Orange, Michael M. Angell, John R. Brand, Jim Thomson, Tim Buddin, Mark Williams, William Hart, William J. Berger, III
Publisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 5–8, 2003
Paper Number: OTC-15157-MS
... Abstract Both the Mad Dog and Atlantis field development areas (southeast Green Canyon) extend across the Sigsbee Escarpment, the surface and seaward-most manifestation of mobile salt in the northern Gulf of Mexico. Understanding the shallow geologic setting of the Sigsbee Escarpment...
Proceedings Papers
Tectonic Control of Early Cretaceous Carbonate Platforms in the Gulf of Mexico
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 1–4, 1995
Paper Number: OTC-7690-MS
.... Atlantic hinge zone formation to a change in spreadinglocus that occurred halfway through the rift stage of basin evolution. Initially, spreading occurred landward of the future hinge zone then moved seaward of it, resulting in two spatially separated phases of extension and subsidence. Crust landward...
Proceedings Papers
Resolution: A Key to Better Understanding Continental Slope and Rise Processes, U.S. Atlantic Continental Margin
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 7–9, 1984
Paper Number: OTC-4722-MS
... seaward oceanographer canyon submarine canyon reservoir characterization shelf edge canyon wall canyon sea floor morphology geology OTC 4722 Resolution: A Key to Better Understanding Continental Slope and Rise Processes, U.S. Atlantic Continental Margin by B.A. McGregor, USGS 1 This paper...
Proceedings Papers
Seafloor Geologic Hazards in OCS Lease Area 55, Eastern Gulf of Alaska
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 5–8, 1980
Paper Number: OTC-3914-MS
.... Gas charged sediments are common near the Alsek and Dangerous Rivers and also occur elsewhere in the region. These rivers are major sources of sediment and may be transporting to their fullest during times of glacial-lake "breakouts." Buried channels are most prevalent seaward of these rivers and off...
Proceedings Papers
Permafrost Beneath The Beaufort Sea: Near Prudhoe Bay, Alaska
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, April 30–May 3, 1979
Paper Number: OTC-3527-MS
... subsea permafrost. prudhoe bay engineering property upstream oil & gas fine-grained sediment seaward sediment permafrost kpa temperature profile gravel alaska perennially reservoir characterization beaufort sea penetrometer water content resistance strength us government...
Proceedings Papers
Deformation And Origin Of The Sigsbee Scarp-Lower Continental Slope, Northern Gulf Of Mexico
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 7–10, 1978
Paper Number: OTC-3217-MS
... Fan suggest salt movement here is mainly vertical in nature. The Sigsbee Scarp is formed by the seaward most of a series of salt ridges that have uplifted and deformed Pleistocene sediments. The Scarp continues eastward beneath the Mississippi Fan but loses its topographic expression and is buried...
Proceedings Papers
Integrated Environmental Studies, South Texas Outer Continental Shelf: Approach, Techniques, Results
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 1–4, 1977
Paper Number: OTC-2754-MS
... of the water from mid shelf seaward to the edge of the shelf at mid and near-bottom depths is locally very high and a supersaturated condition is indicated. Geologically, the shelf has undergone seaward tilting or subsidence as a continuing process. The subsidence has been accompanied by extensive faulting...
Proceedings Papers
Geology Of The Bering Shelf
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 1–4, 1977
Paper Number: OTC-2727-MS
... American plate was a subduction zone. interior salt basin aleutian island tertiary basin alaska otc 2727 seaward kula plate reservoir characterization upstream oil & gas george basin subduction zone navarin basin freeworld oil company fragment oceanic plate structural geology...
Proceedings Papers
Stamukhi Zone Processes: Implications For Developing The Arctic Offshore
Available to PurchasePublisher: Offshore Technology Conference
Paper presented at the Offshore Technology Conference, May 1–4, 1977
Paper Number: OTC-2945-MS
... and shear ridges as well as hummock fields form along the boundary and are stabilized by grounding, generally between the 10- to 20-m isobaths. Slippage along this boundary occurs intermittently at or seaward of the grounded ridges, forming new grounded ridge systems in a widening zone - the saluki zone...