Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway

The Vestertana Group in East Finnmark, North Norway, contains two Neoproterozoic glaciogenic sequences, the Smalfjord and Mortensnes formations, preserved on the northern edge of Baltica. The former comprises up to 420 m of aeolian, fluvioglacial and glaciomarine sediments and terrestrial diamictite...

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Published in:Geological Society, London, Memoirs
Main Authors: Rice, Alexander Hugh N., Edwards, Marc B., Hansen, Tor A., Arnaud, Emmanuelle, Halverson, Galen Pippa
Other Authors: School of Earth and Environmental Sciences
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/2440/74256
https://doi.org/10.1144/M36.57
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/74256
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/74256 2023-05-15T16:13:37+02:00 Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway Rice, Alexander Hugh N. Edwards, Marc B. Hansen, Tor A. Arnaud, Emmanuelle Halverson, Galen Pippa School of Earth and Environmental Sciences 2012 http://hdl.handle.net/2440/74256 https://doi.org/10.1144/M36.57 en eng Geological Society, London, Memoirs, 2012; 36(1):593-602 0435-4052 http://hdl.handle.net/2440/74256 doi:10.1144/M36.57 © The Geological Society of London 2011 Journal article 2012 ftunivadelaidedl https://doi.org/10.1144/M36.57 2023-02-05T19:41:37Z The Vestertana Group in East Finnmark, North Norway, contains two Neoproterozoic glaciogenic sequences, the Smalfjord and Mortensnes formations, preserved on the northern edge of Baltica. The former comprises up to 420 m of aeolian, fluvioglacial and glaciomarine sediments and terrestrial diamictite. The latter consists of up to 50 m of predominantly diamictite. The Smalfjord Formation (Fm.) is underlain by dolostones (Grasdalen Fm., Tanafjorden Group), only locally preserved due to the sub-Smalfjord Fm. unconformity, which cuts down-section through a c. 2.5 km dominantly clastic sequence to rest on Baltic Shield gneisses. The two glaciogenic successions are separated by c. 350 m of mostly clastic sediments (Nyborg Fm.), with thin dolostones at the base and towards the top. The latter are generally absent due to the sub-Mortensnes Fm. unconformity, which also cuts down southwards through the Nyborg and Smalfjord formations to the Baltic Shield. No robust isotopic age constraints are available for the succession. δ13C data, together with cap dolostone characteristics, offer paradigmic correlations with other areas (Smalfjord ≡ Marinoan; Mortensnes ≡ Gaskiers). A limited Ediacaran fauna, including Aspidella, give only broad age constraints. Palaeomagnetic data are ambiguous; some suggest Baltica lay at equatorial (15°S) to mid-latitudes (50°S) for the period 750–550 Ma, respectively, while other interpretations place it at either 30°N or S at c. 550 Ma. A. Hugh N. Rice, Marc B. Edwards, Tor A. Hansen, Emmanuelle Arnaud and Galen P. Halverson Article in Journal/Newspaper Finnmark North Norway Finnmark The University of Adelaide: Digital Library Mortensnes ENVELOPE(20.269,20.269,69.581,69.581) Norway Smalfjord ENVELOPE(28.062,28.062,70.439,70.439) Tanafjorden ENVELOPE(28.391,28.391,70.747,70.747) Vestertana ENVELOPE(27.868,27.868,70.424,70.424) Geological Society, London, Memoirs 36 1 593 602
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
description The Vestertana Group in East Finnmark, North Norway, contains two Neoproterozoic glaciogenic sequences, the Smalfjord and Mortensnes formations, preserved on the northern edge of Baltica. The former comprises up to 420 m of aeolian, fluvioglacial and glaciomarine sediments and terrestrial diamictite. The latter consists of up to 50 m of predominantly diamictite. The Smalfjord Formation (Fm.) is underlain by dolostones (Grasdalen Fm., Tanafjorden Group), only locally preserved due to the sub-Smalfjord Fm. unconformity, which cuts down-section through a c. 2.5 km dominantly clastic sequence to rest on Baltic Shield gneisses. The two glaciogenic successions are separated by c. 350 m of mostly clastic sediments (Nyborg Fm.), with thin dolostones at the base and towards the top. The latter are generally absent due to the sub-Mortensnes Fm. unconformity, which also cuts down southwards through the Nyborg and Smalfjord formations to the Baltic Shield. No robust isotopic age constraints are available for the succession. δ13C data, together with cap dolostone characteristics, offer paradigmic correlations with other areas (Smalfjord ≡ Marinoan; Mortensnes ≡ Gaskiers). A limited Ediacaran fauna, including Aspidella, give only broad age constraints. Palaeomagnetic data are ambiguous; some suggest Baltica lay at equatorial (15°S) to mid-latitudes (50°S) for the period 750–550 Ma, respectively, while other interpretations place it at either 30°N or S at c. 550 Ma. A. Hugh N. Rice, Marc B. Edwards, Tor A. Hansen, Emmanuelle Arnaud and Galen P. Halverson
author2 School of Earth and Environmental Sciences
format Article in Journal/Newspaper
author Rice, Alexander Hugh N.
Edwards, Marc B.
Hansen, Tor A.
Arnaud, Emmanuelle
Halverson, Galen Pippa
spellingShingle Rice, Alexander Hugh N.
Edwards, Marc B.
Hansen, Tor A.
Arnaud, Emmanuelle
Halverson, Galen Pippa
Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
author_facet Rice, Alexander Hugh N.
Edwards, Marc B.
Hansen, Tor A.
Arnaud, Emmanuelle
Halverson, Galen Pippa
author_sort Rice, Alexander Hugh N.
title Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
title_short Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
title_full Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
title_fullStr Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
title_full_unstemmed Glaciogenic rocks of the Neoproterozoic Smalfjord and Mortensnes formations, Vestertana Group, E. Finnmark, Norway
title_sort glaciogenic rocks of the neoproterozoic smalfjord and mortensnes formations, vestertana group, e. finnmark, norway
publishDate 2012
url http://hdl.handle.net/2440/74256
https://doi.org/10.1144/M36.57
long_lat ENVELOPE(20.269,20.269,69.581,69.581)
ENVELOPE(28.062,28.062,70.439,70.439)
ENVELOPE(28.391,28.391,70.747,70.747)
ENVELOPE(27.868,27.868,70.424,70.424)
geographic Mortensnes
Norway
Smalfjord
Tanafjorden
Vestertana
geographic_facet Mortensnes
Norway
Smalfjord
Tanafjorden
Vestertana
genre Finnmark
North Norway
Finnmark
genre_facet Finnmark
North Norway
Finnmark
op_relation Geological Society, London, Memoirs, 2012; 36(1):593-602
0435-4052
http://hdl.handle.net/2440/74256
doi:10.1144/M36.57
op_rights © The Geological Society of London 2011
op_doi https://doi.org/10.1144/M36.57
container_title Geological Society, London, Memoirs
container_volume 36
container_issue 1
container_start_page 593
op_container_end_page 602
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