The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen

Abstract The Lower Old Red Sandstone deposits of Ekmanfjorden belong mainly to the Lykta Division, but pale sandstones with Giganthaspis representingthe Kapp Kjeldsen Division also occur in the core of what is probably a N.-S. striking anticline. The lower beds of the Lykta Division are soft, dull a...

Full description

Bibliographic Details
Published in:Geological Magazine
Main Author: Dineley, D. L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1960
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800061045
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061045
id crcambridgeupr:10.1017/s0016756800061045
record_format openpolar
spelling crcambridgeupr:10.1017/s0016756800061045 2024-09-15T18:04:31+00:00 The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen Dineley, D. L. 1960 http://dx.doi.org/10.1017/s0016756800061045 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061045 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 97, issue 1, page 18-32 ISSN 0016-7568 1469-5081 journal-article 1960 crcambridgeupr https://doi.org/10.1017/s0016756800061045 2024-07-31T04:01:29Z Abstract The Lower Old Red Sandstone deposits of Ekmanfjorden belong mainly to the Lykta Division, but pale sandstones with Giganthaspis representingthe Kapp Kjeldsen Division also occur in the core of what is probably a N.-S. striking anticline. The lower beds of the Lykta Division are soft, dull and silty and not very fossiliferous; above them are some 1,100 feet of sandstones and conglomeratic beds alternatingwith shales or marls. Locally abundant vertebrate remains include the guide fossil Doryaspis . Various sedimentary structures suggest rapid deposition on a broad shallow delta front. Article in Journal/Newspaper Ekmanfjord* Cambridge University Press Geological Magazine 97 1 18 32
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The Lower Old Red Sandstone deposits of Ekmanfjorden belong mainly to the Lykta Division, but pale sandstones with Giganthaspis representingthe Kapp Kjeldsen Division also occur in the core of what is probably a N.-S. striking anticline. The lower beds of the Lykta Division are soft, dull and silty and not very fossiliferous; above them are some 1,100 feet of sandstones and conglomeratic beds alternatingwith shales or marls. Locally abundant vertebrate remains include the guide fossil Doryaspis . Various sedimentary structures suggest rapid deposition on a broad shallow delta front.
format Article in Journal/Newspaper
author Dineley, D. L.
spellingShingle Dineley, D. L.
The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
author_facet Dineley, D. L.
author_sort Dineley, D. L.
title The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
title_short The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
title_full The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
title_fullStr The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
title_full_unstemmed The Old Red Sandstone of Eastern Ekmanfjorden, Vestspitsbergen
title_sort old red sandstone of eastern ekmanfjorden, vestspitsbergen
publisher Cambridge University Press (CUP)
publishDate 1960
url http://dx.doi.org/10.1017/s0016756800061045
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061045
genre Ekmanfjord*
genre_facet Ekmanfjord*
op_source Geological Magazine
volume 97, issue 1, page 18-32
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800061045
container_title Geological Magazine
container_volume 97
container_issue 1
container_start_page 18
op_container_end_page 32
_version_ 1810442008361172992