Thickness and distribution of sedimentary rocks in the southern Barents Sea.

The southern Barents Sea is underlain by sediments of varying thickness and physical properties. The thick sequence of Tertiary sedimentary rocks, which is representative of the southern provinces of the Norwegian continental margin, is found only as a wedge near the shelf edge of the Barents Sea. S...

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Bibliographic Details
Main Author: Sundvor, Eirik
Format: Article in Journal/Newspaper
Language:English
Published: 1975
Subjects:
SEDIMENTÆR BERGART
SEDIMENTOLOGI
Barents Sea
Tromsøflaket
Online Access:https://hdl.handle.net/11250/2675017
id ftnorgesgu:oai:openarchive.ngu.no:11250/2675017
record_format openpolar
spelling ftnorgesgu:oai:openarchive.ngu.no:11250/2675017 2023-05-15T15:38:00+02:00 Thickness and distribution of sedimentary rocks in the southern Barents Sea. Sundvor, Eirik 1975 application/pdf https://hdl.handle.net/11250/2675017 eng eng NGU (316) https://hdl.handle.net/11250/2675017 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 237-240 SEDIMENTÆR BERGART SEDIMENTOLOGI Journal article 1975 ftnorgesgu 2022-07-03T15:26:22Z The southern Barents Sea is underlain by sediments of varying thickness and physical properties. The thick sequence of Tertiary sedimentary rocks, which is representative of the southern provinces of the Norwegian continental margin, is found only as a wedge near the shelf edge of the Barents Sea. Structures that can be associated with salt diapirs are recorded in a limited area on Tromsøflaket. 35908 Article in Journal/Newspaper Barents Sea Tromsøflaket NGU Open Archive (Geological Survey of Norway) Barents Sea Tromsøflaket ENVELOPE(18.500,18.500,71.500,71.500)
institution Open Polar
collection NGU Open Archive (Geological Survey of Norway)
op_collection_id ftnorgesgu
language English
topic SEDIMENTÆR BERGART
SEDIMENTOLOGI
spellingShingle SEDIMENTÆR BERGART
SEDIMENTOLOGI
Sundvor, Eirik
Thickness and distribution of sedimentary rocks in the southern Barents Sea.
topic_facet SEDIMENTÆR BERGART
SEDIMENTOLOGI
description The southern Barents Sea is underlain by sediments of varying thickness and physical properties. The thick sequence of Tertiary sedimentary rocks, which is representative of the southern provinces of the Norwegian continental margin, is found only as a wedge near the shelf edge of the Barents Sea. Structures that can be associated with salt diapirs are recorded in a limited area on Tromsøflaket. 35908
format Article in Journal/Newspaper
author Sundvor, Eirik
author_facet Sundvor, Eirik
author_sort Sundvor, Eirik
title Thickness and distribution of sedimentary rocks in the southern Barents Sea.
title_short Thickness and distribution of sedimentary rocks in the southern Barents Sea.
title_full Thickness and distribution of sedimentary rocks in the southern Barents Sea.
title_fullStr Thickness and distribution of sedimentary rocks in the southern Barents Sea.
title_full_unstemmed Thickness and distribution of sedimentary rocks in the southern Barents Sea.
title_sort thickness and distribution of sedimentary rocks in the southern barents sea.
publishDate 1975
url https://hdl.handle.net/11250/2675017
long_lat ENVELOPE(18.500,18.500,71.500,71.500)
geographic Barents Sea
Tromsøflaket
geographic_facet Barents Sea
Tromsøflaket
genre Barents Sea
Tromsøflaket
genre_facet Barents Sea
Tromsøflaket
op_source 237-240
op_relation NGU (316)
https://hdl.handle.net/11250/2675017
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
op_rightsnorm CC-BY
_version_ 1766368696245157888

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