Petrography and diagenesis of the Triassic and Jurassic sandstones, eastern part of the Norwegian-Danish Basin

Rikke Weibel; Mette Olivarius; Lars Henrik Nielsen; Tanni Abramovitz; Claus Kjøller

doi:10.22008/gpub/28449

Petrography and diagenesis of the Triassic and Jurassic sandstones, eastern part of the Norwegian-Danish Basin

Rikke Weibel, Mette Olivarius, Lars Henrik Nielsen, Tanni Abramovitz, Claus Kjøller

Publikation: Bog/rapport › Rapport (offentligt tilgængelig)

Resumé

The most prominent clastic reservoir rocks in eastern part of the Norwegian-Danish Basin (onshore Denmark) are the Triassic-Jurassoc sediments comprising the Bunter Sandstone Formation, Skagerrak Formation, Gassum Formation and the Haldager Sand Formation. The Bunter Sandstone Formation is deposited by ephemeral streams, terminal fans or aeolian activity in an arid (hot) climate. The Skagerrak Formation comprises sediments from alluvial fans grading into braided streams. The lower part of the Skagerrak Formation is northern equivalent to the Bunter Sandstone Formation occurring mainly south of the Ringkøbing-Fyn High, whereas the upper part is contemporaneous with the Gassum Formation. The Gassum Formation and the Haldager Sand formations are deposited in fluvial, parallic and shallow marine environment under humid and vegetated conditions.

Originalsprog	Engelsk
Udgivelsessted	Copenhagen
Forlag	GEUS
Antal sider	83
Vol/bind	2011
DOI	https://doi.org/10.22008/gpub/28449
Status	Udgivet - 26 jan. 2011

Publikationsserier

Navn	Danmarks og Grønlands Geologiske Undersøgelse Rapport
Nummer	5
Vol/bind	2011

Emneord

Denmark

Programområde

Programområde 3: Energiressourcer

Adgang til dokumentet

10.22008/gpub/28449Licens: Ikke-specificeret

https://data.geus.dk/pure-pdf/28449_GEUS-R_2011_5_opt.pdfLicens: Ikke-specificeret

Citationsformater

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title = "Petrography and diagenesis of the Triassic and Jurassic sandstones, eastern part of the Norwegian-Danish Basin",

abstract = "The most prominent clastic reservoir rocks in eastern part of the Norwegian-Danish Basin (onshore Denmark) are the Triassic-Jurassoc sediments comprising the Bunter Sandstone Formation, Skagerrak Formation, Gassum Formation and the Haldager Sand Formation. The Bunter Sandstone Formation is deposited by ephemeral streams, terminal fans or aeolian activity in an arid (hot) climate. The Skagerrak Formation comprises sediments from alluvial fans grading into braided streams. The lower part of the Skagerrak Formation is northern equivalent to the Bunter Sandstone Formation occurring mainly south of the Ringk{\o}bing-Fyn High, whereas the upper part is contemporaneous with the Gassum Formation. The Gassum Formation and the Haldager Sand formations are deposited in fluvial, parallic and shallow marine environment under humid and vegetated conditions.",

keywords = "Denmark, Denmark",

author = "Rikke Weibel and Mette Olivarius and Nielsen, {Lars Henrik} and Tanni Abramovitz and Claus Kj{\o}ller",

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doi = "10.22008/gpub/28449",

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AU - Weibel, Rikke

AU - Olivarius, Mette

AU - Nielsen, Lars Henrik

AU - Abramovitz, Tanni

AU - Kjøller, Claus

PY - 2011/1/26

Y1 - 2011/1/26

N2 - The most prominent clastic reservoir rocks in eastern part of the Norwegian-Danish Basin (onshore Denmark) are the Triassic-Jurassoc sediments comprising the Bunter Sandstone Formation, Skagerrak Formation, Gassum Formation and the Haldager Sand Formation. The Bunter Sandstone Formation is deposited by ephemeral streams, terminal fans or aeolian activity in an arid (hot) climate. The Skagerrak Formation comprises sediments from alluvial fans grading into braided streams. The lower part of the Skagerrak Formation is northern equivalent to the Bunter Sandstone Formation occurring mainly south of the Ringkøbing-Fyn High, whereas the upper part is contemporaneous with the Gassum Formation. The Gassum Formation and the Haldager Sand formations are deposited in fluvial, parallic and shallow marine environment under humid and vegetated conditions.

AB - The most prominent clastic reservoir rocks in eastern part of the Norwegian-Danish Basin (onshore Denmark) are the Triassic-Jurassoc sediments comprising the Bunter Sandstone Formation, Skagerrak Formation, Gassum Formation and the Haldager Sand Formation. The Bunter Sandstone Formation is deposited by ephemeral streams, terminal fans or aeolian activity in an arid (hot) climate. The Skagerrak Formation comprises sediments from alluvial fans grading into braided streams. The lower part of the Skagerrak Formation is northern equivalent to the Bunter Sandstone Formation occurring mainly south of the Ringkøbing-Fyn High, whereas the upper part is contemporaneous with the Gassum Formation. The Gassum Formation and the Haldager Sand formations are deposited in fluvial, parallic and shallow marine environment under humid and vegetated conditions.

KW - Denmark

U2 - 10.22008/gpub/28449

DO - 10.22008/gpub/28449

M3 - Report (publicly available)

VL - 2011

T3 - Danmarks og Grønlands Geologiske Undersøgelse Rapport

BT - Petrography and diagenesis of the Triassic and Jurassic sandstones, eastern part of the Norwegian-Danish Basin

PB - GEUS

CY - Copenhagen

ER -

Petrography and diagenesis of the Triassic and Jurassic sandstones, eastern part of the Norwegian-Danish Basin

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