Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf.

Eckart Hakansson; Lars Stemmerik

doi:10.1007/978-94-009-5626-1_8

Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf.

Eckart Hakansson, Lars Stemmerik

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

52 Citationer (Scopus)

Resumé

A composite sequence totalling well over 7km has been recorded, which gives evidence for a complex depositional and structural history of the basin encompassing the Carboniferous to Tertiary interval. Depositional environments in the Carboniferous to Triassic, as well as in the Palaeocene, compare well with the situation recorded in Svalbard. During the late Cretaceous, several pull-apart basins were filled and deformed in a dextral strike-slip mobile belt, largely paralleling the subsequent suture between Greenland and Svalbard. The type of deposition in individual basins varies widely. Some contain fluvial-deltaic and marine sediments whereas a single basin is dominated by continental vulcanogenic sediments and extrusives.-from Authors

Originalsprog	Engelsk
Titel	Petroleum Geology of the North European Margin
Undertitel	Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983
Redaktører	A.M. Spencer
Forlag	Springer
Sider	97-107
Antal sider	11
ISBN (Elektronisk)	978-94-009-5626-1
ISBN (Trykt)	978-0-86010-486-5
DOI	https://doi.org/10.1007/978-94-009-5626-1_8
Status	Udgivet - 1984
Udgivet eksternt	Ja
Begivenhed	North European Margin Symposium 1983 - Norwegian Institute of Technology, Trondheim, Norge Varighed: 9 maj 1983 → 11 maj 1983

Konference

Konference	North European Margin Symposium 1983
Forkortet titel	NEMS '83
Land/Område	Norge
By	Trondheim
Periode	9/05/83 → 11/05/83

Programområde

Programområde 3: Energiressourcer

FN’s Verdensmål

Dette resultat bidrager til følgende verdensmål

Adgang til dokumentet

10.1007/978-94-009-5626-1_8

Citationsformater

Hakansson, E., & Stemmerik, L. (1984). Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf. I A. M. Spencer (red.), Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983 (s. 97-107). Springer. https://doi.org/10.1007/978-94-009-5626-1_8

Hakansson, Eckart ; Stemmerik, Lars. / Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf. Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983. red. / A.M. Spencer. Springer, 1984. s. 97-107

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title = "Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf.",

abstract = "A composite sequence totalling well over 7km has been recorded, which gives evidence for a complex depositional and structural history of the basin encompassing the Carboniferous to Tertiary interval. Depositional environments in the Carboniferous to Triassic, as well as in the Palaeocene, compare well with the situation recorded in Svalbard. During the late Cretaceous, several pull-apart basins were filled and deformed in a dextral strike-slip mobile belt, largely paralleling the subsequent suture between Greenland and Svalbard. The type of deposition in individual basins varies widely. Some contain fluvial-deltaic and marine sediments whereas a single basin is dominated by continental vulcanogenic sediments and extrusives.-from Authors",

author = "Eckart Hakansson and Lars Stemmerik",

year = "1984",

doi = "10.1007/978-94-009-5626-1_8",

language = "English",

isbn = "978-0-86010-486-5",

pages = "97--107",

editor = "Spencer, {A.M. }",

booktitle = "Petroleum Geology of the North European Margin",

publisher = "Springer",

address = "China",

note = "North European Margin Symposium 1983, NEMS '83 ; Conference date: 09-05-1983 Through 11-05-1983",

}

Hakansson, E & Stemmerik, L 1984, Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf. i AM Spencer (red.), Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983. Springer, s. 97-107, North European Margin Symposium 1983, Trondheim, Norge, 9/05/83. https://doi.org/10.1007/978-94-009-5626-1_8

Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf. / Hakansson, Eckart; Stemmerik, Lars.
Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983. red. / A.M. Spencer. Springer, 1984. s. 97-107.

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

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AU - Hakansson, Eckart

AU - Stemmerik, Lars

PY - 1984

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N2 - A composite sequence totalling well over 7km has been recorded, which gives evidence for a complex depositional and structural history of the basin encompassing the Carboniferous to Tertiary interval. Depositional environments in the Carboniferous to Triassic, as well as in the Palaeocene, compare well with the situation recorded in Svalbard. During the late Cretaceous, several pull-apart basins were filled and deformed in a dextral strike-slip mobile belt, largely paralleling the subsequent suture between Greenland and Svalbard. The type of deposition in individual basins varies widely. Some contain fluvial-deltaic and marine sediments whereas a single basin is dominated by continental vulcanogenic sediments and extrusives.-from Authors

AB - A composite sequence totalling well over 7km has been recorded, which gives evidence for a complex depositional and structural history of the basin encompassing the Carboniferous to Tertiary interval. Depositional environments in the Carboniferous to Triassic, as well as in the Palaeocene, compare well with the situation recorded in Svalbard. During the late Cretaceous, several pull-apart basins were filled and deformed in a dextral strike-slip mobile belt, largely paralleling the subsequent suture between Greenland and Svalbard. The type of deposition in individual basins varies widely. Some contain fluvial-deltaic and marine sediments whereas a single basin is dominated by continental vulcanogenic sediments and extrusives.-from Authors

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Hakansson E, Stemmerik L. Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf. I Spencer AM, red., Petroleum Geology of the North European Margin: Proceedings of the North European Margin Symposium (NEMS '83), organized by the Norwegian Petroleum Society and held at the Norwegian Institute of Technology (NTH) in Trondheim 9–11 May, 1983. Springer. 1984. s. 97-107 doi: 10.1007/978-94-009-5626-1_8

Wandel Sea Basin - the North Greenland equivalent to Svalbard and the Barents Shelf.

Resumé

Konference

Programområde

FN’s Verdensmål

Adgang til dokumentet

Fingeraftryk

Citationsformater