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Showing 1 to 6 of 6 for “"seismics"”.
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Geomorphologic Evaluation of the Gulf of Mexico, Northwest Garden Banks, and Supra/Inter/Subsalt Architectural Influences on Possible Reservoir Characterization from the Miocene to Pleistocene Epochs
… less precise, are used in conjunction with 3D seismics for an overview of the surrounding area. Some logs are used in conjunction with the seismics for upper Miocene to Pleistocene control. This geologic re-evaluation of the Gulf of Mexico, Garden Banks field 236 and a one to three block …
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Data adaptive velocity/depth spectra estimation in seismic wide angle reflection analysis
In studying the earth with reflection seismics, one of the major unknowns is the velocity structure of the medium. Techniques used to determine the velocity structure commonly involve multi-channel arrays which measure the spatial as well as the time structure of the returning signals. The …
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Investigating Mesoscale, Submesoscale, and Mixing Ocean Dynamics in the Mozambique Channel Using Seismic and Simulation Datasets
… study mesoscale-submesoscale interactions using seismics: here water masses from the Indian and Atlantic ocean collide and interact, driving sharp thermohaline gradients and intense current flows interact with complex bathymetry to produce an energetic eddy field. First, a standard processing …
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Combination of Borehole Seismic and Downhole Logging to Investigate the Vicinity of the COSC‑1 Borehole in Western Scandinavia
In dieser Arbeit werden bohrlochseismsiche Messungen sowohl mit Bohrlochmessungen als auch mit oberflächenseismischen Messungen ausgewertet und verglichen um das bohrlochnahe Umfeld der Forschungsbohrung COSC-1 (Collisional Orogeny in the Scandinavian Caledonides) zu beschreiben. Die …
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Seismic reflection imaging of near surface structures using the Common Reflection Surface (CRS) Stack Method
… method for use in shallow and ultrashallow seismics.
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Seismic structure of the Arava Fault, Dead Sea Transform
Ein transversales Störungssystem im Nahen Osten, die Dead Sea Transform (DST), trennt die Arabische Platte von der Sinai-Mikroplatte und erstreckt sich von Süden nach Norden vom Extensionsgebiet im Roten Meer über das Tote Meer bis zur Taurus-Zagros Kollisionszone. Die sinistrale DST bildete sich …