Tom Bendiksen 37 p 4. The dimensions of the ridges are: height 40 m, length 2—4. The hydrate zone may have thicken. The onset of the Lofoten Drift may have be. The Lofoten Contourite Drift is located below c. The discovery record so far is much in favour of.
Marine environments, ranging from neritic to bathyal water depths, dominated the southern Bare. Steinar Øksenvåg vant selve finalen med 38 poeng foran Morten Gjønnes og Tom Bendiksen på 37 poeng. The drift probably originated from the deposition of suspended sediments derived from winnowing of the shelf and upper sl. Seismic reflection data and well logs are used to interpret Cenozoic sedimentary environments in the southwestern Barents Sea. We have a tradition of working closely together with international partners, in particular Russian scientists having key data and knowledge about the eastern, central and northern Barents Sea. Morten Gjønnes 37 p 3.
Using seismic stratigraphy combined with information from 24 wells, a detailed history of the early Cenozoic sedimentation of the Hammerfest Basin in the southwestern Barents Sea has been revealed. Seismic reflection data and well logs are used to interpret Cenozoic sedimentary environments in the south-western Barents Sea. By sequence stratigraphic analysis of seismic data from the western Barents Shelf, nine sequences from late Miocene to Pleistocene are discussed. På kvelden var det trivelig bankett for 65 deltakere med stor premieutdeling på Hjelseng gård. The understanding of the regional geology and tectonic evolution in the Barents Sea region will be enhanced. . Touren har gått over 20 uker i perioden april til september hvorav de 7 beste rundene har vært tellende i sammendraget.
Vinnere: Topp 5 Finale se golfbox for fullstendig resultatliste 1. The new, partly quantitative, understanding of basin development and petroleum systems will provide a better basis to assess the petroleum potential and reduce exploration risk in the north. On the southwestern Barents Sea shelf, sediments containing gas hydrates that overlie free gas have been inferred from multichannel seismic data. Seismic interpretation and mapping of the Sørvestsnaget Basin at the southwestern Barents Sea Margin has revealed a complex basin history, related to large scale plate tectonic movements in the Norwegian-Greenland Sea area. Spilleformen er stableford så alle uansett hcp har hatt mulighet til å vinne. The sequences reflect a generally aggradational and progradational period of the shelf, and by using global eustatic curves they are tentatively proposed to be deposited from 5. The sequences comprises mainly lowstand fans and lowstand prograding complexes whereas the transgressive and highstand systems tracts are largely missing due to erosion.
Based on high-resolution and multichannel seismic data, a contourite drift, the Lofoten Drift, has been identified below ca. Velkommen til Stjørdal Golf Tour 2018. The Lofoten Drift has a maximum thickness of about 360 m. Bengt Klefbom 36 p 5. The Neogene strata are dominated by contourites related to the ocean circulation established from.
After exploring the southern part of the Norwegian Barents Sea referred to as the Barents Sea for simplicity throughout rest of the paper for almost 20 years, operating 18 wells and participating in another 22 wells, Norsk Hydro in 1996-1997 reviewed the engagement and remaining oil prospectivity. It has a maximum thickness of about 360 m and correlation to published seismic stratigraphy implies a Neogene age. This erosion occurred during mid Miocene to mid Pleistocene periods of low relative sea-level stand. From 2D and 3D seismic mapping, the western Barents Sea continental margin development shows a complex history of structural configuration of highs and basins related to the Greenland. The Cenozoic pre-glacial development of the southwestern Barents Sea is discussed, with focus on the early to middle Cenozoic net erosion that was poorly constrained. During the early Paleocene the Hammerfest Basin was subject to non-deposition or minor erosion, and sedimentation in the basin was initiated after a tran. Using volumetric calculations and compaction trend analysis, the Cenozoic erosion and sedimentation rates have been quantified.
By volumetric calculation we have quantified the Cenozoic erosion and sedimentation rates. This paper discusses six mid and upper Miocene seismic stratigraphic sequences. The gas hydrate zone probably formed from thermogenic gas leaking from a deeper source. The pre-Cenozoic evolution of the Sørvestsnaget Basin is poorly understood, due to lack of well data and poor seismic data qual. In the Svalbard area close to 3000 meters have been eroded sinc. The overall Cenozoic erosion varies spatially as well as temporally.
The volume of suspected gas hydrate is tentatively estimated to about 1. Correlation to published seismic stratigraphy implies a Neogene age. . . . . .
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