A shoshonitic dyke in Lohja, Southern Finland

We describe here a newly discovered cross-cutting mafic dyke in the vicinity of Lohja, southern Finland. The dyke is E-W trending and about 6 m in width. Only a few zircons were recovered from the dyke despite the high Zr contents and they all were inherited. Therefore, the crystallisation age remai...

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Main Authors: Hugh O’Brien, Jaakko Kara, Marek Lehtinen, Markku Väisänen, Marja Lehtonen
Other Authors: geologia, Geology, 2606902
Language:English
Published: Suomi 2022
Subjects:
Online Access:https://www.utupub.fi/handle/10024/161662
http://www.seismo.helsinki.fi/pdf/Lito2016.pdf
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spelling ftunivturku:oai:www.utupub.fi:10024/161662 2023-05-15T16:11:42+02:00 A shoshonitic dyke in Lohja, Southern Finland Lithosphere 2016: Ninth symposium on the Structure, Composition and Evolution of the Lithosphere in Fennoscandia Hugh O’Brien Jaakko Kara Marek Lehtinen Markku Väisänen Marja Lehtonen geologia, Geology 2606902 2022-10-28T12:43:57Z 74 71 https://www.utupub.fi/handle/10024/161662 http://www.seismo.helsinki.fi/pdf/Lito2016.pdf en eng Suomi Finland FI Helsinki Report - institute of seismology. university of helsinki. s 65 Lithosphere Report - Institute of seismology. University of helsinki 978-952-10-9588-7 https://www.utupub.fi/handle/10024/161662 http://www.seismo.helsinki.fi/pdf/Lito2016.pdf URN:NBN:fi-fe2021042715684 978-952-10-9589-4 0357-3060 2022 ftunivturku 2022-11-03T00:00:22Z We describe here a newly discovered cross-cutting mafic dyke in the vicinity of Lohja, southern Finland. The dyke is E-W trending and about 6 m in width. Only a few zircons were recovered from the dyke despite the high Zr contents and they all were inherited. Therefore, the crystallisation age remains uncertain. The dyke is shoshonitic in composition and the closest analogues are the åva lamprophyre dykes in SW Finland. Other/Unknown Material Fennoscandia University of Turku: UTUPub
institution Open Polar
collection University of Turku: UTUPub
op_collection_id ftunivturku
language English
description We describe here a newly discovered cross-cutting mafic dyke in the vicinity of Lohja, southern Finland. The dyke is E-W trending and about 6 m in width. Only a few zircons were recovered from the dyke despite the high Zr contents and they all were inherited. Therefore, the crystallisation age remains uncertain. The dyke is shoshonitic in composition and the closest analogues are the åva lamprophyre dykes in SW Finland.
author2 geologia, Geology
2606902
author Hugh O’Brien
Jaakko Kara
Marek Lehtinen
Markku Väisänen
Marja Lehtonen
spellingShingle Hugh O’Brien
Jaakko Kara
Marek Lehtinen
Markku Väisänen
Marja Lehtonen
A shoshonitic dyke in Lohja, Southern Finland
author_facet Hugh O’Brien
Jaakko Kara
Marek Lehtinen
Markku Väisänen
Marja Lehtonen
author_sort Hugh O’Brien
title A shoshonitic dyke in Lohja, Southern Finland
title_short A shoshonitic dyke in Lohja, Southern Finland
title_full A shoshonitic dyke in Lohja, Southern Finland
title_fullStr A shoshonitic dyke in Lohja, Southern Finland
title_full_unstemmed A shoshonitic dyke in Lohja, Southern Finland
title_sort shoshonitic dyke in lohja, southern finland
publisher Suomi
publishDate 2022
url https://www.utupub.fi/handle/10024/161662
http://www.seismo.helsinki.fi/pdf/Lito2016.pdf
genre Fennoscandia
genre_facet Fennoscandia
op_relation Report - institute of seismology. university of helsinki. s
65
Lithosphere
Report - Institute of seismology. University of helsinki
978-952-10-9588-7
https://www.utupub.fi/handle/10024/161662
http://www.seismo.helsinki.fi/pdf/Lito2016.pdf
URN:NBN:fi-fe2021042715684
978-952-10-9589-4
0357-3060
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