Alloktone aflejringer i Maastrichtien kalken på Mors

E. Nygaard; Peter Frykman

Alloktone aflejringer i Maastrichtien kalken på Mors

Publikation: Bidrag til tidsskrift › Artikel › Forskning › peer review

3 Citationer (Scopus)

Resumé

Allochthonous deposits are demonstrated in the Maastrichtian succession of pelagic white chalk from the Erslev 3S well. These deposits are conglomerates of chalk pebbles supported by a contorted matrix and are interpreted to be allochthonous units deposited as debris-flows. One unit attains a minimum thickness of 1.25m. A possible trigger for this type of deposition is thought to be a phase of active diapirism in the underlying salt piercement dome.

Bidragets oversatte titel	Allochthonous deposits in the Maastrichtian chalk of the island of Mors, northern Denmark
Originalsprog	Dansk
Sider (fra-til)	57-60
Antal sider	4
Tidsskrift	Årsskrift for Dansk geologisk Forening
Vol/bind	1980
Status	Udgivet - 25 jan. 1981

Programområde

Programområde 3: Energiressourcer

Adgang til dokumentet

https://2dgf.dk/xpdf/dgfaars1980-57-60.pdfLicens: Ikke-specificeret

Citationsformater

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abstract = "Allochthonous deposits are demonstrated in the Maastrichtian succession of pelagic white chalk from the Erslev 3S well. These deposits are conglomerates of chalk pebbles supported by a contorted matrix and are interpreted to be allochthonous units deposited as debris-flows. One unit attains a minimum thickness of 1.25m. A possible trigger for this type of deposition is thought to be a phase of active diapirism in the underlying salt piercement dome.",

keywords = "Chalk",

author = "E. Nygaard and Peter Frykman",

year = "1981",

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TY - JOUR

T1 - Alloktone aflejringer i Maastrichtien kalken på Mors

AU - Nygaard, E.

AU - Frykman, Peter

PY - 1981/1/25

Y1 - 1981/1/25

N2 - Allochthonous deposits are demonstrated in the Maastrichtian succession of pelagic white chalk from the Erslev 3S well. These deposits are conglomerates of chalk pebbles supported by a contorted matrix and are interpreted to be allochthonous units deposited as debris-flows. One unit attains a minimum thickness of 1.25m. A possible trigger for this type of deposition is thought to be a phase of active diapirism in the underlying salt piercement dome.

AB - Allochthonous deposits are demonstrated in the Maastrichtian succession of pelagic white chalk from the Erslev 3S well. These deposits are conglomerates of chalk pebbles supported by a contorted matrix and are interpreted to be allochthonous units deposited as debris-flows. One unit attains a minimum thickness of 1.25m. A possible trigger for this type of deposition is thought to be a phase of active diapirism in the underlying salt piercement dome.

KW - Chalk

UR - https://www.scopus.com/pages/publications/0019749407

M3 - Artikel

AN - SCOPUS:0019749407

VL - 1980

SP - 57

EP - 60

JO - Årsskrift for Dansk geologisk Forening

JF - Årsskrift for Dansk geologisk Forening

ER -

Alloktone aflejringer i Maastrichtien kalken på Mors

Resumé

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