Optimizing Deepwater Well Locations To Reduce the Risk of Shallow-Water-Flow Using High-Resolution 2D and 3D Seismic Data

2000 ◽  
Author(s):  
Daniel R. McConnell
Keyword(s):  
High Resolution ◽  
Shallow Water ◽  
Water Flow ◽  
Seismic Data ◽  
3D Seismic ◽  
Shallow Water Flow ◽  
2D And 3D ◽  
3D Seismic Data

scholarly journals High-resolution landform assemblage along a buried glacio-erosive surface in the SW Barents Sea revealed by P-Cable 3D seismic data

Geomorphology ◽  
2019 ◽  
Vol 332 ◽  
pp. 33-50 ◽  
Author(s):  
Benjamin Bellwald ◽  
Sverre Planke ◽  
Nina Lebedeva-Ivanova ◽  
Emilia D. Piasecka ◽  
Karin Andreassen
Keyword(s):  
High Resolution ◽  
Seismic Data ◽  
Barents Sea ◽  
3D Seismic ◽  
3D Seismic Data

Quaternary evolution of the northern North Sea

2020 ◽  
Author(s):  
Christine Batchelor ◽  
Dag Ottesen ◽  
Benjamin Bellwald ◽  
Sverre Planke ◽  
Helge Løseth ◽  
...  
Keyword(s):  
North Sea ◽  
Seismic Data ◽  
3D Seismic ◽  
Quaternary Sediments ◽  
The North ◽  
The North Sea ◽  
Data Coverage ◽  
Northern North Sea ◽  
2D And 3D ◽  
3D Seismic Data

<p>The North Sea has arguably the most extensive geophysical data coverage of any glacier-influenced sedimentary regime on Earth, enabling detailed investigation of the thick (up to 1 km) sequence of Quaternary sediments that is preserved within the North Sea Basin. At the start of the Quaternary, the bathymetry of the northern North Sea was dominated by a deep depression that provided accommodation for sediment input from the Norwegian mainland and the East Shetland Platform. Here we use an extensive database of 2D and 3D seismic data to investigate the geological development of the northern North Sea through the Quaternary.</p><p>Three main sedimentary processes were dominant within the northern North Sea during the early Quaternary: 1) the delivery and associated basinward transfer of glacier-derived sediments from an ice mass centred over mainland Norway; 2) the delivery of fluvio-deltaic sediments from the East Shetland Platform; and 3) contourite deposition and the reworking of sediments by contour currents. The infilling of the North Sea Basin during the early Quaternary increased the width and reduced the water depth of the continental shelf, facilitating the initiation of the Norwegian Channel Ice Stream.</p>

Iceberg ploughmarks in the SW Barents Sea imaged using high-resolution P-Cable 3D seismic data

2016 ◽  
Vol 46 (1) ◽  
pp. 281-282 ◽  
Author(s):  
S. Vadakkepuliyambatta ◽  
S. Bünz ◽  
A. Tasianas ◽  
J. Mienert
Keyword(s):  
High Resolution ◽  
Seismic Data ◽  
Barents Sea ◽  
3D Seismic ◽  
3D Seismic Data
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