Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian

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Standard

Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian. / Clemmensen, Lars B.; Bromley, Richard Granville; Holm, Paul Martin.

I: Bulletin of the Geological Society of Denmark, Bind 59, 02.2011, s. 1-12.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Clemmensen, LB, Bromley, RG & Holm, PM 2011, 'Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian', Bulletin of the Geological Society of Denmark, bind 59, s. 1-12. <http://2dgf.dk/xpdf/bull59-1-12.pdf>

APA

Clemmensen, L. B., Bromley, R. G., & Holm, P. M. (2011). Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian. Bulletin of the Geological Society of Denmark, 59, 1-12. http://2dgf.dk/xpdf/bull59-1-12.pdf

Vancouver

Clemmensen LB, Bromley RG, Holm PM. Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian. Bulletin of the Geological Society of Denmark. 2011 feb.;59:1-12.

Author

Clemmensen, Lars B. ; Bromley, Richard Granville ; Holm, Paul Martin. / Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian. I: Bulletin of the Geological Society of Denmark. 2011 ; Bind 59. s. 1-12.

Bibtex

@article{4c751f734d3d4c55a55ef92d67c2a7f4,
title = "Glauconitic deposits at Juleg{\aa}rd on the south coast of Bornholm, Denmark dated to the Cambrian",
abstract = "Bioturbated, glauconitic siltstones and sandstones are overlain by presumed Upper Triassic deposits at coastal exposures at Juleg{\aa}rd on the south coast of Bornholm. These glauconitic deposits have not previously been dated. A 40Ar-39Ar dating of the glaucony gives an age of 493 ± 2 Ma suggesting the deposits belong to the Lower Cambrian Norretorp Member of the L{\ae}s{\aa} Formation. The shallow marine deposits are strongly bioturbated, but only a single ichnoassociation is represented. The ichnogenus is referable to either Trichophycus Miller and Dyer, 1878 or Teichichnus Seilacher, 1955. Rare examples of Rusophycus Hall, 1852, probably trilobite trace fossils, are also represented.",
author = "Clemmensen, {Lars B.} and Bromley, {Richard Granville} and Holm, {Paul Martin}",
year = "2011",
month = feb,
language = "English",
volume = "59",
pages = "1--12",
journal = "Bulletin of the Geological Society of Denmark",
issn = "0011-6297",
publisher = "Dansk Geologisk Forening",

}

RIS

TY - JOUR

T1 - Glauconitic deposits at Julegård on the south coast of Bornholm, Denmark dated to the Cambrian

AU - Clemmensen, Lars B.

AU - Bromley, Richard Granville

AU - Holm, Paul Martin

PY - 2011/2

Y1 - 2011/2

N2 - Bioturbated, glauconitic siltstones and sandstones are overlain by presumed Upper Triassic deposits at coastal exposures at Julegård on the south coast of Bornholm. These glauconitic deposits have not previously been dated. A 40Ar-39Ar dating of the glaucony gives an age of 493 ± 2 Ma suggesting the deposits belong to the Lower Cambrian Norretorp Member of the Læså Formation. The shallow marine deposits are strongly bioturbated, but only a single ichnoassociation is represented. The ichnogenus is referable to either Trichophycus Miller and Dyer, 1878 or Teichichnus Seilacher, 1955. Rare examples of Rusophycus Hall, 1852, probably trilobite trace fossils, are also represented.

AB - Bioturbated, glauconitic siltstones and sandstones are overlain by presumed Upper Triassic deposits at coastal exposures at Julegård on the south coast of Bornholm. These glauconitic deposits have not previously been dated. A 40Ar-39Ar dating of the glaucony gives an age of 493 ± 2 Ma suggesting the deposits belong to the Lower Cambrian Norretorp Member of the Læså Formation. The shallow marine deposits are strongly bioturbated, but only a single ichnoassociation is represented. The ichnogenus is referable to either Trichophycus Miller and Dyer, 1878 or Teichichnus Seilacher, 1955. Rare examples of Rusophycus Hall, 1852, probably trilobite trace fossils, are also represented.

M3 - Journal article

VL - 59

SP - 1

EP - 12

JO - Bulletin of the Geological Society of Denmark

JF - Bulletin of the Geological Society of Denmark

SN - 0011-6297

ER -

ID: 34253559