Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen

Pyroclastic material of a rhyolite type is present in some thin layers in the upper part of the De Geerdalen Formation in the Sassenfjorden area. This is the first evidence of late Triassic (Norian.Rhaetian) volcanic activity in Svalbard.

Bibliographic Details
Published in:Polar Research
Main Authors: Chlebowski, Roman, Wierzbowski, Andrzej
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2010
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2546
https://doi.org/10.3402/polar.v1i1.6971
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spelling ftjpolarres:oai:journals.openacademia.net:article/2546 2023-05-15T18:02:40+02:00 Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen Chlebowski, Roman Wierzbowski, Andrzej 2010-01-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2546 https://doi.org/10.3402/polar.v1i1.6971 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2546/5797 https://polarresearch.net/index.php/polar/article/view/2546 doi:10.3402/polar.v1i1.6971 Copyright (c) 2018 Polar Research Polar Research; Vol. 1 No. 1 (1983); 75-81 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2010 ftjpolarres https://doi.org/10.3402/polar.v1i1.6971 2021-11-11T19:12:57Z Pyroclastic material of a rhyolite type is present in some thin layers in the upper part of the De Geerdalen Formation in the Sassenfjorden area. This is the first evidence of late Triassic (Norian.Rhaetian) volcanic activity in Svalbard. Article in Journal/Newspaper Polar Research Sassenfjord* Sassenfjorden Svalbard Spitsbergen Polar Research (E-Journal) Svalbard De Geerdalen ENVELOPE(16.368,16.368,78.296,78.296) Sassenfjorden ENVELOPE(16.217,16.217,78.412,78.412) Polar Research 1 1 75 81
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description Pyroclastic material of a rhyolite type is present in some thin layers in the upper part of the De Geerdalen Formation in the Sassenfjorden area. This is the first evidence of late Triassic (Norian.Rhaetian) volcanic activity in Svalbard.
format Article in Journal/Newspaper
author Chlebowski, Roman
Wierzbowski, Andrzej
spellingShingle Chlebowski, Roman
Wierzbowski, Andrzej
Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
author_facet Chlebowski, Roman
Wierzbowski, Andrzej
author_sort Chlebowski, Roman
title Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
title_short Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
title_full Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
title_fullStr Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
title_full_unstemmed Pyroclastic material from the Upper Triassic deposits of Sassenfjorden, Spitsbergen
title_sort pyroclastic material from the upper triassic deposits of sassenfjorden, spitsbergen
publisher Norwegian Polar Institute
publishDate 2010
url https://polarresearch.net/index.php/polar/article/view/2546
https://doi.org/10.3402/polar.v1i1.6971
long_lat ENVELOPE(16.368,16.368,78.296,78.296)
ENVELOPE(16.217,16.217,78.412,78.412)
geographic Svalbard
De Geerdalen
Sassenfjorden
geographic_facet Svalbard
De Geerdalen
Sassenfjorden
genre Polar Research
Sassenfjord*
Sassenfjorden
Svalbard
Spitsbergen
genre_facet Polar Research
Sassenfjord*
Sassenfjorden
Svalbard
Spitsbergen
op_source Polar Research; Vol. 1 No. 1 (1983); 75-81
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2546/5797
https://polarresearch.net/index.php/polar/article/view/2546
doi:10.3402/polar.v1i1.6971
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v1i1.6971
container_title Polar Research
container_volume 1
container_issue 1
container_start_page 75
op_container_end_page 81
_version_ 1766173107026919424