Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland

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Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland. / Piasecki, Stefan; Bojesen-Koefoed, Jorgen A.; Alsen, Peter.

In: Bulletin of the Geological Society of Denmark, Vol. 68, 2020, p. 155-169.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Piasecki, S, Bojesen-Koefoed, JA & Alsen, P 2020, 'Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland', Bulletin of the Geological Society of Denmark, vol. 68, pp. 155-169. https://doi.org/10.37570/bgsd-2020-68-07

APA

Piasecki, S., Bojesen-Koefoed, J. A., & Alsen, P. (2020). Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland. Bulletin of the Geological Society of Denmark, 68, 155-169. https://doi.org/10.37570/bgsd-2020-68-07

Vancouver

Piasecki S, Bojesen-Koefoed JA, Alsen P. Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland. Bulletin of the Geological Society of Denmark. 2020;68:155-169. https://doi.org/10.37570/bgsd-2020-68-07

Author

Piasecki, Stefan ; Bojesen-Koefoed, Jorgen A. ; Alsen, Peter. / Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland. In: Bulletin of the Geological Society of Denmark. 2020 ; Vol. 68. pp. 155-169.

Bibtex

@article{9a31f87e96a14a4a9658c618b41f9a1e,
title = "Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland",
abstract = "New data on the Lower Cretaceous Falskebugt Member (Palnatokes Bjerg Formation) and Stratumbjerg Formation in easternmost Wollaston Forland, northern East Greenland, are interpreted here. The type locality of the Falskebugt Member on the north-west corner of the Falkebjerg ridge has been revisited, and additional new good exposures were found in a riverbed just north of Falkebjerg and more in river beds on the plain further to the north, where both the Falskebugt Member and the Stratumbjerg Formation are exposed. Previously, only a limited marine fauna was reported providing a restricted middle Valanginian age of the Falskebugt Member. New fossil faunas in other parts of the Falskebugt Member suggest an early Valanginian - Hauterivian age and confirm lateral correlation with the Albrechts Bugt and Rodryggen Members of the Palnatokes Bjerg Formation. However, in places where the Falskebugt Member is exposed in contact with the lower Stratumbjerg Formation, dinoflagellate cysts from these units indicate Barremian and late Barremian ages, respectively. The stratigraphic range of the combined biostratigraphic data from the Falskebugt Member indicates an early Valanginian - late Barremian age. Dinoflagellate cysts from part of the assemblage in the Stratumbjerg Formation suggest a marginal marine/brackish water depositional environment. Comparable depositional environments are also recorded in upper Barremian sediments on Store Koldewey and in the Ladegardsaen Formation on Peary Land much farther to the north in Greenland. The dark mudstones of the Stratumbjerg Formation show no potential for generation of liquid hydrocarbons, and the immature and poorly sorted sediments of the Falskebugt Member have little potential as a petroleum reservoir.",
keywords = "Stratigraphy, ammonites, dinoflagellate cysts, geochemistry, Falskebugt Member, Stratumbjerg Formation, Cretaceous, East Greenland, BIOSTRATIGRAPHY",
author = "Stefan Piasecki and Bojesen-Koefoed, {Jorgen A.} and Peter Alsen",
year = "2020",
doi = "10.37570/bgsd-2020-68-07",
language = "English",
volume = "68",
pages = "155--169",
journal = "Bulletin of the Geological Society of Denmark",
issn = "0011-6297",
publisher = "Dansk Geologisk Forening",

}

RIS

TY - JOUR

T1 - Geology of the Lower Cretaceous in the Falkebjerg area, Wollaston Forland, northern East Greenland

AU - Piasecki, Stefan

AU - Bojesen-Koefoed, Jorgen A.

AU - Alsen, Peter

PY - 2020

Y1 - 2020

N2 - New data on the Lower Cretaceous Falskebugt Member (Palnatokes Bjerg Formation) and Stratumbjerg Formation in easternmost Wollaston Forland, northern East Greenland, are interpreted here. The type locality of the Falskebugt Member on the north-west corner of the Falkebjerg ridge has been revisited, and additional new good exposures were found in a riverbed just north of Falkebjerg and more in river beds on the plain further to the north, where both the Falskebugt Member and the Stratumbjerg Formation are exposed. Previously, only a limited marine fauna was reported providing a restricted middle Valanginian age of the Falskebugt Member. New fossil faunas in other parts of the Falskebugt Member suggest an early Valanginian - Hauterivian age and confirm lateral correlation with the Albrechts Bugt and Rodryggen Members of the Palnatokes Bjerg Formation. However, in places where the Falskebugt Member is exposed in contact with the lower Stratumbjerg Formation, dinoflagellate cysts from these units indicate Barremian and late Barremian ages, respectively. The stratigraphic range of the combined biostratigraphic data from the Falskebugt Member indicates an early Valanginian - late Barremian age. Dinoflagellate cysts from part of the assemblage in the Stratumbjerg Formation suggest a marginal marine/brackish water depositional environment. Comparable depositional environments are also recorded in upper Barremian sediments on Store Koldewey and in the Ladegardsaen Formation on Peary Land much farther to the north in Greenland. The dark mudstones of the Stratumbjerg Formation show no potential for generation of liquid hydrocarbons, and the immature and poorly sorted sediments of the Falskebugt Member have little potential as a petroleum reservoir.

AB - New data on the Lower Cretaceous Falskebugt Member (Palnatokes Bjerg Formation) and Stratumbjerg Formation in easternmost Wollaston Forland, northern East Greenland, are interpreted here. The type locality of the Falskebugt Member on the north-west corner of the Falkebjerg ridge has been revisited, and additional new good exposures were found in a riverbed just north of Falkebjerg and more in river beds on the plain further to the north, where both the Falskebugt Member and the Stratumbjerg Formation are exposed. Previously, only a limited marine fauna was reported providing a restricted middle Valanginian age of the Falskebugt Member. New fossil faunas in other parts of the Falskebugt Member suggest an early Valanginian - Hauterivian age and confirm lateral correlation with the Albrechts Bugt and Rodryggen Members of the Palnatokes Bjerg Formation. However, in places where the Falskebugt Member is exposed in contact with the lower Stratumbjerg Formation, dinoflagellate cysts from these units indicate Barremian and late Barremian ages, respectively. The stratigraphic range of the combined biostratigraphic data from the Falskebugt Member indicates an early Valanginian - late Barremian age. Dinoflagellate cysts from part of the assemblage in the Stratumbjerg Formation suggest a marginal marine/brackish water depositional environment. Comparable depositional environments are also recorded in upper Barremian sediments on Store Koldewey and in the Ladegardsaen Formation on Peary Land much farther to the north in Greenland. The dark mudstones of the Stratumbjerg Formation show no potential for generation of liquid hydrocarbons, and the immature and poorly sorted sediments of the Falskebugt Member have little potential as a petroleum reservoir.

KW - Stratigraphy

KW - ammonites

KW - dinoflagellate cysts

KW - geochemistry

KW - Falskebugt Member

KW - Stratumbjerg Formation

KW - Cretaceous

KW - East Greenland

KW - BIOSTRATIGRAPHY

U2 - 10.37570/bgsd-2020-68-07

DO - 10.37570/bgsd-2020-68-07

M3 - Journal article

VL - 68

SP - 155

EP - 169

JO - Bulletin of the Geological Society of Denmark

JF - Bulletin of the Geological Society of Denmark

SN - 0011-6297

ER -

ID: 247543759