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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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 |
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Open Polar |
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University of Turku: UTUPub |
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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 |
_version_ |
1765996859236548608 |