By Norsk petroleumsforening. Conference, Ole J. Martinsen, Tom Dreyer
ISBN-10: 0444502416
ISBN-13: 9780444502414
Required examining for geologists operating within the offshore parts, quantity 10 maintains the sequence from the Norwegian Petroleum Society. This paintings presents an up to date assessment of the past due Palaeozoic to offer sedimentary heritage of the Norwegian offshore components within the North Sea and Mid-Norway basins. Case reports, assessment articles and analogue examples from adjoining parts resembling Greenland and Denmark, current new rules at the improvement of the Norwegian margin from the Carboniferous during the Mesozoic and Cenozoic.In specific, new proof and interpretations are awarded on famous significant reservoir-bearing successions equivalent to the Statfjord Formation and Dunlin crew within the Northern North Sea, and the Åre and the Tilje Formations within the Mid-Norway zone. additionally, the higher Jurassic succession within the Haltenbanken region is defined, giving new facts at the interaction among extensional tectonics and sedimentation throughout the moment significant rift section within the area.The Cretaceous and Cenozoic sessions are taken care of widely, displaying their significance as total deep water sedimentary structures with confirmed and strength reservoir rocks, similar to within the Ormen Lange box, and for inflicting burial of Jurassic rocks to effective depths for hydrocarbon iteration. the hot sedimentary historical past of the Norwegian margin is taken care of with examples of the glacial heritage and sizeable submarine slides which knowing is essential for the situation of offshore installations.The booklet is organised in response to geologic time, from Palaeozoic via Mesozoic to Cenozoic examples. It encompasses a set of palaeogeographic maps from the Carboniferous via to the Cenozoic. furthermore, there are various examples of center photos, good log info, correlation panels and seismic in addition to outcrop images and logs from the analogue examples. finished reference and key-phrase lists also are incorporated.
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Additional resources for Sedimentary environments offshore Norway--Palaeozoic to Recent: proceedings of the Norwegian Petroleum Society Conference, 3-5 May 1999, Bergen, Norway
Sample text
Subsequent to the latest Paleocene/earliest Eocene voluminous break-up magmatism the newly established spreading axis and surrounding lava platforms started to subside and eventually became submerged. The main part of the Eocene succession is a slope/basin floor system downlapping and thinning towards the east throughout the northern North Sea and the MOre Basin. , 1999). , 1988). , 1993a). The Paleocene to Oligocene environments of Svalbard were much more complex because of the involvement in the Spitsbergen Orogeny (Fig.
The global sea level continued to rise until its maximum in the middle of Campanian times. This was the time span of the mature Chalk Sea that also transgressed the crystalline basement of southern Norway and southem Sweden (Riis, 1996) (Fig. 21). The increased area of submergence caused the mature Chalk Sea to produce carbonates of higher purity than the early Chalk Sea. The general deposits of the chalk seas were a combination of bioturbated homogenised chalk ooze and downslope redeposited, better sorted ooze.
The palaeogeography of Barremian times plotted on the 70 Ma plate reconstruction. Some key references for compilation: Dalland (1981); Hfikansson and Stemmerik (1984); Steel and Worsley (1984); Ziegler (1988); Surlyk (1990); Dor6 (1992); N~attvedt et al. (1993a); Johansen et al. (1993); Stemmerik et al. (1993); Oakman and Partington (1998); Larsen et al. (1999); Brekke et al. (1999); supplemented by in-house studies. See Fig. 5b for legend. areas and in starved distal deeps, was halted by a sudden sea-level drop at the peak of the Barremian high-stand.
Sedimentary environments offshore Norway--Palaeozoic to Recent: proceedings of the Norwegian Petroleum Society Conference, 3-5 May 1999, Bergen, Norway by Norsk petroleumsforening. Conference, Ole J. Martinsen, Tom Dreyer
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