Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen
It has been previously suggested that the high-pressure metamorphic rock complcx of Motalafjclla. central-western Spitsbergen, is older than Lower Silurian. An unconformity has been discovered at the base of a limestone which contains fossils similar to those reported as Lower Silurian from the same...
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Norwegian Polar Institute
2010
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ftjpolarres:oai:journals.openacademia.net:article/2560 2023-05-15T18:02:40+02:00 Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen Ohta, Yoshihide Hiroi, Yoshikuni Hirajima, Takao 2010-01-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2560 https://doi.org/10.3402/polar.v1i2.6986 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2560/5811 https://polarresearch.net/index.php/polar/article/view/2560 doi:10.3402/polar.v1i2.6986 Copyright (c) 2018 Polar Research Polar Research; Vol. 1 No. 2 (1983); 215-218 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2010 ftjpolarres https://doi.org/10.3402/polar.v1i2.6986 2021-11-11T19:12:57Z It has been previously suggested that the high-pressure metamorphic rock complcx of Motalafjclla. central-western Spitsbergen, is older than Lower Silurian. An unconformity has been discovered at the base of a limestone which contains fossils similar to those reported as Lower Silurian from the same massif. This proves that the high-pressure metamorphics represent an older rock complex. The unconformity surfacc is invcrted in the area, and large recumbent folds involving the Silurian Bulltindcn Formation havc been mapped. These folds are considered to be prc-Carboniferous Article in Journal/Newspaper Polar Research Spitsbergen Polar Research (E-Journal) Polar Research 1 2 215 218 |
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Open Polar |
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Polar Research (E-Journal) |
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ftjpolarres |
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English |
description |
It has been previously suggested that the high-pressure metamorphic rock complcx of Motalafjclla. central-western Spitsbergen, is older than Lower Silurian. An unconformity has been discovered at the base of a limestone which contains fossils similar to those reported as Lower Silurian from the same massif. This proves that the high-pressure metamorphics represent an older rock complex. The unconformity surfacc is invcrted in the area, and large recumbent folds involving the Silurian Bulltindcn Formation havc been mapped. These folds are considered to be prc-Carboniferous |
format |
Article in Journal/Newspaper |
author |
Ohta, Yoshihide Hiroi, Yoshikuni Hirajima, Takao |
spellingShingle |
Ohta, Yoshihide Hiroi, Yoshikuni Hirajima, Takao Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
author_facet |
Ohta, Yoshihide Hiroi, Yoshikuni Hirajima, Takao |
author_sort |
Ohta, Yoshihide |
title |
Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
title_short |
Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
title_full |
Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
title_fullStr |
Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
title_full_unstemmed |
Additional evidence of pre-Silurian high-pressure metamorphic rocks in Spitsbergen |
title_sort |
additional evidence of pre-silurian high-pressure metamorphic rocks in spitsbergen |
publisher |
Norwegian Polar Institute |
publishDate |
2010 |
url |
https://polarresearch.net/index.php/polar/article/view/2560 https://doi.org/10.3402/polar.v1i2.6986 |
genre |
Polar Research Spitsbergen |
genre_facet |
Polar Research Spitsbergen |
op_source |
Polar Research; Vol. 1 No. 2 (1983); 215-218 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2560/5811 https://polarresearch.net/index.php/polar/article/view/2560 doi:10.3402/polar.v1i2.6986 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v1i2.6986 |
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Polar Research |
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1 |
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2 |
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215 |
op_container_end_page |
218 |
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1766173108146798592 |