Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland

The existence of alum shale in the small Finnish sector of the Scandinavian Caledonides has been verified by chemical finds. Enhanced values for V and Mo (1050 and 450 ppm, respectively) together with more common tenors of C and U have been reported. These values could be used to discriminate betwee...

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Bibliographic Details
Main Author: Jyrki J Lehtovaara
Format: Article in Journal/Newspaper
Language:English
Published: Geographical Society of Finland 1986
Subjects:
geo
Online Access:https://doaj.org/article/fb76fc5537ee42b19a70dd1f9c759708
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:fb76fc5537ee42b19a70dd1f9c759708 2023-05-15T16:06:12+02:00 Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland Jyrki J Lehtovaara 1986-01-01 https://doaj.org/article/fb76fc5537ee42b19a70dd1f9c759708 en eng Geographical Society of Finland 1798-5617 https://doaj.org/article/fb76fc5537ee42b19a70dd1f9c759708 undefined Fennia: International Journal of Geography, Vol 164, Iss 1 (1986) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1986 fttriple 2023-01-22T19:15:49Z The existence of alum shale in the small Finnish sector of the Scandinavian Caledonides has been verified by chemical finds. Enhanced values for V and Mo (1050 and 450 ppm, respectively) together with more common tenors of C and U have been reported. These values could be used to discriminate between the alum shale and common black shale otherwise similar in appearance. The find was made in the only slightly metamorphosed lower­most unit of the Caledonide overthrust plates, the Jerta Nappe. This provides further proof of the only parautochthonous character of this nappe and also of the continuity of the alum shale sedimentary facies along the eastern margin of the Caledonides. Article in Journal/Newspaper Enontekiö Lapland Unknown Enontekiö ENVELOPE(23.632,23.632,68.386,68.386)
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Jyrki J Lehtovaara
Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
topic_facet geo
description The existence of alum shale in the small Finnish sector of the Scandinavian Caledonides has been verified by chemical finds. Enhanced values for V and Mo (1050 and 450 ppm, respectively) together with more common tenors of C and U have been reported. These values could be used to discriminate between the alum shale and common black shale otherwise similar in appearance. The find was made in the only slightly metamorphosed lower­most unit of the Caledonide overthrust plates, the Jerta Nappe. This provides further proof of the only parautochthonous character of this nappe and also of the continuity of the alum shale sedimentary facies along the eastern margin of the Caledonides.
format Article in Journal/Newspaper
author Jyrki J Lehtovaara
author_facet Jyrki J Lehtovaara
author_sort Jyrki J Lehtovaara
title Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
title_short Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
title_full Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
title_fullStr Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
title_full_unstemmed Traces of alum shale in the Finnish Caledonides of the Enontekiö Lapland
title_sort traces of alum shale in the finnish caledonides of the enontekiö lapland
publisher Geographical Society of Finland
publishDate 1986
url https://doaj.org/article/fb76fc5537ee42b19a70dd1f9c759708
long_lat ENVELOPE(23.632,23.632,68.386,68.386)
geographic Enontekiö
geographic_facet Enontekiö
genre Enontekiö
Lapland
genre_facet Enontekiö
Lapland
op_source Fennia: International Journal of Geography, Vol 164, Iss 1 (1986)
op_relation 1798-5617
https://doaj.org/article/fb76fc5537ee42b19a70dd1f9c759708
op_rights undefined
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