VK2021-Sabina-AKTW.pdf
The Alta–Kvænangen Tectonic Window (AKTW) is one of several terrains in northern Norway that represent a north-western continuation of the Precambrian Fennoscandian Shield beneath the Scandinavian Caledonides. The supracrustal complex of AKTW is similar to those of other tectonic windows in northern...
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Vinterkonferansen 2021
2021
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ftdatacite:10.6084/m9.figshare.13525460.v1 2023-05-15T16:12:51+02:00 VK2021-Sabina-AKTW.pdf Palinkas, Sabina S Hansen, Harald Sondre Stenvold Simonsen Hilmo, Johan Bang Faber, Carly Sahlström, Fredrik Mun, Yulia Bergh, Steffen G. Spangenberg, Jorge E 2021 https://dx.doi.org/10.6084/m9.figshare.13525460.v1 https://ngf-vk21.figshare.com/articles/poster/VK2021-Sabina-AKTW_pdf/13525460/1 unknown Vinterkonferansen 2021 https://dx.doi.org/10.6084/m9.figshare.13525460 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY 40201 Exploration Geochemistry FOS Earth and related environmental sciences 40307 Ore Deposit Petrology 40299 Geochemistry not elsewhere classified Image graphic Poster ImageObject 2021 ftdatacite https://doi.org/10.6084/m9.figshare.13525460.v1 https://doi.org/10.6084/m9.figshare.13525460 2021-11-05T12:55:41Z The Alta–Kvænangen Tectonic Window (AKTW) is one of several terrains in northern Norway that represent a north-western continuation of the Precambrian Fennoscandian Shield beneath the Scandinavian Caledonides. The supracrustal complex of AKTW is similar to those of other tectonic windows in northern Norway, including Repparfjord Tectonic Window and Alteneset Tectonic Window, and it is predominantly composed of mafic lavas and mafic tuffs, intrusive gabbro-dolerite sills, minor ultramafic rocks and carbonate-rich metasedimentary rocks. In contrast to other tectonic windows in northern Norway, AKTW has not been a subject of intensive deformation processes (Bergh & Torske, 1988; Melezhik et al., 2015). Therefore, AKTW represents an ideal area to study lithostratigraphic features of Precambrian metavolcano-sedimentary complexes in the Fennoscandian Shield as well as associated ore-forming processes. Still Image Fennoscandian Kvænangen Northern Norway DataCite Metadata Store (German National Library of Science and Technology) Alta Alteneset ENVELOPE(23.042,23.042,70.327,70.327) Kvænangen ENVELOPE(21.726,21.726,69.931,69.931) Norway Repparfjord ENVELOPE(24.550,24.550,70.417,70.417) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
40201 Exploration Geochemistry FOS Earth and related environmental sciences 40307 Ore Deposit Petrology 40299 Geochemistry not elsewhere classified |
spellingShingle |
40201 Exploration Geochemistry FOS Earth and related environmental sciences 40307 Ore Deposit Petrology 40299 Geochemistry not elsewhere classified Palinkas, Sabina S Hansen, Harald Sondre Stenvold Simonsen Hilmo, Johan Bang Faber, Carly Sahlström, Fredrik Mun, Yulia Bergh, Steffen G. Spangenberg, Jorge E VK2021-Sabina-AKTW.pdf |
topic_facet |
40201 Exploration Geochemistry FOS Earth and related environmental sciences 40307 Ore Deposit Petrology 40299 Geochemistry not elsewhere classified |
description |
The Alta–Kvænangen Tectonic Window (AKTW) is one of several terrains in northern Norway that represent a north-western continuation of the Precambrian Fennoscandian Shield beneath the Scandinavian Caledonides. The supracrustal complex of AKTW is similar to those of other tectonic windows in northern Norway, including Repparfjord Tectonic Window and Alteneset Tectonic Window, and it is predominantly composed of mafic lavas and mafic tuffs, intrusive gabbro-dolerite sills, minor ultramafic rocks and carbonate-rich metasedimentary rocks. In contrast to other tectonic windows in northern Norway, AKTW has not been a subject of intensive deformation processes (Bergh & Torske, 1988; Melezhik et al., 2015). Therefore, AKTW represents an ideal area to study lithostratigraphic features of Precambrian metavolcano-sedimentary complexes in the Fennoscandian Shield as well as associated ore-forming processes. |
format |
Still Image |
author |
Palinkas, Sabina S Hansen, Harald Sondre Stenvold Simonsen Hilmo, Johan Bang Faber, Carly Sahlström, Fredrik Mun, Yulia Bergh, Steffen G. Spangenberg, Jorge E |
author_facet |
Palinkas, Sabina S Hansen, Harald Sondre Stenvold Simonsen Hilmo, Johan Bang Faber, Carly Sahlström, Fredrik Mun, Yulia Bergh, Steffen G. Spangenberg, Jorge E |
author_sort |
Palinkas, Sabina S |
title |
VK2021-Sabina-AKTW.pdf |
title_short |
VK2021-Sabina-AKTW.pdf |
title_full |
VK2021-Sabina-AKTW.pdf |
title_fullStr |
VK2021-Sabina-AKTW.pdf |
title_full_unstemmed |
VK2021-Sabina-AKTW.pdf |
title_sort |
vk2021-sabina-aktw.pdf |
publisher |
Vinterkonferansen 2021 |
publishDate |
2021 |
url |
https://dx.doi.org/10.6084/m9.figshare.13525460.v1 https://ngf-vk21.figshare.com/articles/poster/VK2021-Sabina-AKTW_pdf/13525460/1 |
long_lat |
ENVELOPE(23.042,23.042,70.327,70.327) ENVELOPE(21.726,21.726,69.931,69.931) ENVELOPE(24.550,24.550,70.417,70.417) |
geographic |
Alta Alteneset Kvænangen Norway Repparfjord |
geographic_facet |
Alta Alteneset Kvænangen Norway Repparfjord |
genre |
Fennoscandian Kvænangen Northern Norway |
genre_facet |
Fennoscandian Kvænangen Northern Norway |
op_relation |
https://dx.doi.org/10.6084/m9.figshare.13525460 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.13525460.v1 https://doi.org/10.6084/m9.figshare.13525460 |
_version_ |
1765998457837846528 |