Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf

Lars Stemmerik; David Worsley

doi:10.1007/978-94-009-1149-9_10

Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf

Lars Stemmerik, David Worsley

Publikation: Bidrag til bog/rapport/konferenceproceedings › Konferenceartikel i proceedings › peer review

64 Citationer (Scopus)

Resumé

The latest Devonian (Fammenian) to late Permian (Kazanian) depositional epoch throughout this vast province was characterized by the development of three major sequences, with boundaries which reflect regional shifts in tectonic, hydrographic and climatic regimes. Upper Devonian to lower Carboniferous fluviatile and lacustrine sequences were deposited in humid conditions before and during early phases of rifting along major sutures in the region. Complex mid-Carboniferous successions display the interplay of active rifting, climatic change and rising sea-level; ongoing sea-level rise and progressively more quiescent tectonic regimes resulted in the regional development of late Carboniferous and early Permian carbonate and evaporite platforms. Short-term sea-level oscillations appear to be responsible for the development of cyclic sequences which can be correlated at several levels in and between these platform environments. Widespread mid-Permian sea-level rise was accompanied by marked changes in depositional style, reflecting major circum-Arctic palaeogeographical realignments and resulting in the third and final sedimentational phase in this epoch. -from Authors

Originalsprog	Engelsk
Titel	Correlation in Petroleum exploration
Undertitel	Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988
Redaktører	John D. Collinson
Udgivelsessted	London
Forlag	Springer
Sider	99-111
Antal sider	13
ISBN (Elektronisk)	978-94-009-1149-9
ISBN (Trykt)	978-94-009-1149-9
DOI	https://doi.org/10.1007/978-94-009-1149-9_10
Status	Udgivet - 1989
Begivenhed	Correlation in Hydrocarbon Exploration - Bergen, Norge Varighed: 3 okt. 1988 → 5 okt. 1988

Konference

Konference	Correlation in Hydrocarbon Exploration
Land/Område	Norge
By	Bergen
Periode	3/10/88 → 5/10/88

Programområde

Programområde 3: Energiressourcer

Adgang til dokumentet

10.1007/978-94-009-1149-9_10

Citationsformater

Stemmerik, L., & Worsley, D. (1989). Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf. I J. D. Collinson (red.), Correlation in Petroleum exploration: Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988 (s. 99-111). Springer. https://doi.org/10.1007/978-94-009-1149-9_10

Stemmerik, Lars ; Worsley, David. / Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf. Correlation in Petroleum exploration: Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988. red. / John D. Collinson. London : Springer, 1989. s. 99-111

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abstract = "The latest Devonian (Fammenian) to late Permian (Kazanian) depositional epoch throughout this vast province was characterized by the development of three major sequences, with boundaries which reflect regional shifts in tectonic, hydrographic and climatic regimes. Upper Devonian to lower Carboniferous fluviatile and lacustrine sequences were deposited in humid conditions before and during early phases of rifting along major sutures in the region. Complex mid-Carboniferous successions display the interplay of active rifting, climatic change and rising sea-level; ongoing sea-level rise and progressively more quiescent tectonic regimes resulted in the regional development of late Carboniferous and early Permian carbonate and evaporite platforms. Short-term sea-level oscillations appear to be responsible for the development of cyclic sequences which can be correlated at several levels in and between these platform environments. Widespread mid-Permian sea-level rise was accompanied by marked changes in depositional style, reflecting major circum-Arctic palaeogeographical realignments and resulting in the third and final sedimentational phase in this epoch. -from Authors",

author = "Lars Stemmerik and David Worsley",

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Stemmerik, L & Worsley, D 1989, Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf. i JD Collinson (red.), Correlation in Petroleum exploration: Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988. Springer, London, s. 99-111, Correlation in Hydrocarbon Exploration, Bergen, Norge, 3/10/88. https://doi.org/10.1007/978-94-009-1149-9_10

Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf. / Stemmerik, Lars; Worsley, David.
Correlation in Petroleum exploration: Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988. red. / John D. Collinson. London: Springer, 1989. s. 99-111.

Publikation: Bidrag til bog/rapport/konferenceproceedings › Konferenceartikel i proceedings › peer review

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N2 - The latest Devonian (Fammenian) to late Permian (Kazanian) depositional epoch throughout this vast province was characterized by the development of three major sequences, with boundaries which reflect regional shifts in tectonic, hydrographic and climatic regimes. Upper Devonian to lower Carboniferous fluviatile and lacustrine sequences were deposited in humid conditions before and during early phases of rifting along major sutures in the region. Complex mid-Carboniferous successions display the interplay of active rifting, climatic change and rising sea-level; ongoing sea-level rise and progressively more quiescent tectonic regimes resulted in the regional development of late Carboniferous and early Permian carbonate and evaporite platforms. Short-term sea-level oscillations appear to be responsible for the development of cyclic sequences which can be correlated at several levels in and between these platform environments. Widespread mid-Permian sea-level rise was accompanied by marked changes in depositional style, reflecting major circum-Arctic palaeogeographical realignments and resulting in the third and final sedimentational phase in this epoch. -from Authors

AB - The latest Devonian (Fammenian) to late Permian (Kazanian) depositional epoch throughout this vast province was characterized by the development of three major sequences, with boundaries which reflect regional shifts in tectonic, hydrographic and climatic regimes. Upper Devonian to lower Carboniferous fluviatile and lacustrine sequences were deposited in humid conditions before and during early phases of rifting along major sutures in the region. Complex mid-Carboniferous successions display the interplay of active rifting, climatic change and rising sea-level; ongoing sea-level rise and progressively more quiescent tectonic regimes resulted in the regional development of late Carboniferous and early Permian carbonate and evaporite platforms. Short-term sea-level oscillations appear to be responsible for the development of cyclic sequences which can be correlated at several levels in and between these platform environments. Widespread mid-Permian sea-level rise was accompanied by marked changes in depositional style, reflecting major circum-Arctic palaeogeographical realignments and resulting in the third and final sedimentational phase in this epoch. -from Authors

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Stemmerik L, Worsley D. Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf. I Collinson JD, red., Correlation in Petroleum exploration: Proceedings of the conference Correlation in Hydrocarbon Exploration organized by the Norwegian Petroleum Society and held in Bergen, Norway, 3–5 October 1988. London: Springer. 1989. s. 99-111 doi: 10.1007/978-94-009-1149-9_10

Late Palaeozoic sequence correlations, North Greenland, Svalbard and the Barents Shelf

Resumé

Konference

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Adgang til dokumentet

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Citationsformater