Oligocene to Holocene

Alan Fyfe; Ulrik Gregersen; Henrik Jordt; Yngve Rundberg; Tor Eidvin; Dan Evans; Derek Stewart; Martin Hovland; Peter Andresen

Oligocene to Holocene

Alan Fyfe, Ulrik Gregersen, Henrik Jordt, Yngve Rundberg, Tor Eidvin, Dan Evans, Derek Stewart, Martin Hovland, Peter Andresen

Afdeling for Geofysik og Sedimentære Bassiner

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

Resumé

The Cenozoic North Sea Basin forms part of the larger Northwest European Basin (Vinken et al., 1988) that extends from the Atlantic shelves of Norway and Shetland in the north-west to the Carpathian Mountains in the south-east. After Eocene times, continuing post-rift subsidence in the North Sea Basin accomodated the deposition of up to 3000 m of Oligocene to Holocene sediments.

Originalsprog	Engelsk
Titel	The Millennium atlas: petroleum geology of the central and northern North Sea
Redaktører	D. Evans, C. Graham, A. Armour, P. Bathurst
Udgivelsessted	London
Forlag	Geological Society of London
Kapitel	16
Sider	279-287
Antal sider	9
Status	Udgivet - 2003

Programområde

Programområde 3: Energiressourcer

Citationsformater

@inbook{e0a9b57f0c1443cea2854a3a0b2ac2f4,

title = "Oligocene to Holocene",

abstract = "The Cenozoic North Sea Basin forms part of the larger Northwest European Basin (Vinken et al., 1988) that extends from the Atlantic shelves of Norway and Shetland in the north-west to the Carpathian Mountains in the south-east. After Eocene times, continuing post-rift subsidence in the North Sea Basin accomodated the deposition of up to 3000 m of Oligocene to Holocene sediments.",

author = "Alan Fyfe and Ulrik Gregersen and Henrik Jordt and Yngve Rundberg and Tor Eidvin and Dan Evans and Derek Stewart and Martin Hovland and Peter Andresen",

year = "2003",

language = "English",

pages = "279--287",

editor = "D. Evans and C. Graham and A. Armour and P. Bathurst",

booktitle = "The Millennium atlas: petroleum geology of the central and northern North Sea",

publisher = "Geological Society of London",

address = "United Kingdom",

}

TY - CHAP

T1 - Oligocene to Holocene

AU - Fyfe, Alan

AU - Gregersen, Ulrik

AU - Jordt, Henrik

AU - Rundberg, Yngve

AU - Eidvin, Tor

AU - Evans, Dan

AU - Stewart, Derek

AU - Hovland, Martin

AU - Andresen, Peter

PY - 2003

Y1 - 2003

N2 - The Cenozoic North Sea Basin forms part of the larger Northwest European Basin (Vinken et al., 1988) that extends from the Atlantic shelves of Norway and Shetland in the north-west to the Carpathian Mountains in the south-east. After Eocene times, continuing post-rift subsidence in the North Sea Basin accomodated the deposition of up to 3000 m of Oligocene to Holocene sediments.

AB - The Cenozoic North Sea Basin forms part of the larger Northwest European Basin (Vinken et al., 1988) that extends from the Atlantic shelves of Norway and Shetland in the north-west to the Carpathian Mountains in the south-east. After Eocene times, continuing post-rift subsidence in the North Sea Basin accomodated the deposition of up to 3000 m of Oligocene to Holocene sediments.

M3 - Chapter in book

SP - 279

EP - 287

BT - The Millennium atlas: petroleum geology of the central and northern North Sea

A2 - Evans, D.

A2 - Graham, C.

A2 - Armour, A.

A2 - Bathurst, P.

PB - Geological Society of London

CY - London

ER -

Oligocene to Holocene

Resumé

Programområde

Fingeraftryk

Citationsformater