Alloktone aflejringer i Maastrichtien kalken på Mors

E. Nygaard; Peter Frykman

Alloktone aflejringer i Maastrichtien kalken på Mors

Translated title of the contribution: Allochthonous deposits in the Maastrichtian chalk of the island of Mors, northern Denmark

E. Nygaard
, Peter Frykman

Research output: Contribution to journal › Article › Research › peer-review

3 Citations (Scopus)

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.

Translated title of the contribution	Allochthonous deposits in the Maastrichtian chalk of the island of Mors, northern Denmark
Original language	Danish
Pages (from-to)	57-60
Number of pages	4
Journal	Årsskrift for Dansk geologisk Forening
Volume	1980
Publication status	Published - 25 Jan 1981

Keywords

Chalk

Programme Area

Programme Area 3: Energy Resources

Access to Document

https://2dgf.dk/xpdf/dgfaars1980-57-60.pdfLicence: Unspecified

Cite this

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title = "Alloktone aflejringer i Maastrichtien kalken p{\aa} Mors",

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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language = "Dansk",

volume = "1980",

pages = "57--60",

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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

Abstract

Keywords

Programme Area

Access to Document

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