Remanent magnetization of two intrusive bodies in southeastern Finland

Direction of natural remanent magnetization (NRM) was measured for a diabase from the intrusive contact of rapakivi granite (1650 Ma) and for a granodiorite intrusion (1810 Ma). The results, although statistically poor, suggest that the apparent polar wandering curve drawn earlier for the Middle Pre...

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Bibliographic Details
Published in:Bulletin of the Geological Society of Finland
Main Author: K.J. Neuvonen
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of Finland 1978
Subjects:
Geology
QE1-996.5
Fennoscandia
Online Access:https://doi.org/10.17741/bgsf/50.1-2.003
https://doaj.org/article/26de9b3fc6674f0b8a7337bcfc48735b
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spelling ftdoajarticles:oai:doaj.org/article:26de9b3fc6674f0b8a7337bcfc48735b 2023-05-15T16:11:39+02:00 Remanent magnetization of two intrusive bodies in southeastern Finland K.J. Neuvonen 1978-12-01T00:00:00Z https://doi.org/10.17741/bgsf/50.1-2.003 https://doaj.org/article/26de9b3fc6674f0b8a7337bcfc48735b EN eng Geological Society of Finland http://www.geologinenseura.fi/bulletin/Volume50/sgs_bt_050_pages_031_037.pdf https://doaj.org/toc/0367-5211 https://doaj.org/toc/1799-4632 doi:10.17741/bgsf/50.1-2.003 0367-5211 1799-4632 https://doaj.org/article/26de9b3fc6674f0b8a7337bcfc48735b Bulletin of the Geological Society of Finland, Vol 50, Iss 1-2, Pp 31-37 (1978) Geology QE1-996.5 article 1978 ftdoajarticles https://doi.org/10.17741/bgsf/50.1-2.003 2022-12-31T04:05:38Z Direction of natural remanent magnetization (NRM) was measured for a diabase from the intrusive contact of rapakivi granite (1650 Ma) and for a granodiorite intrusion (1810 Ma). The results, although statistically poor, suggest that the apparent polar wandering curve drawn earlier for the Middle Precambrian of Fennoscandia from about 2000 to 1200 Ma is correct and not caused by differences in uplift rates. Article in Journal/Newspaper Fennoscandia Directory of Open Access Journals: DOAJ Articles Bulletin of the Geological Society of Finland 50 1-2 31 37
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
K.J. Neuvonen
Remanent magnetization of two intrusive bodies in southeastern Finland
topic_facet Geology
QE1-996.5
description Direction of natural remanent magnetization (NRM) was measured for a diabase from the intrusive contact of rapakivi granite (1650 Ma) and for a granodiorite intrusion (1810 Ma). The results, although statistically poor, suggest that the apparent polar wandering curve drawn earlier for the Middle Precambrian of Fennoscandia from about 2000 to 1200 Ma is correct and not caused by differences in uplift rates.
format Article in Journal/Newspaper
author K.J. Neuvonen
author_facet K.J. Neuvonen
author_sort K.J. Neuvonen
title Remanent magnetization of two intrusive bodies in southeastern Finland
title_short Remanent magnetization of two intrusive bodies in southeastern Finland
title_full Remanent magnetization of two intrusive bodies in southeastern Finland
title_fullStr Remanent magnetization of two intrusive bodies in southeastern Finland
title_full_unstemmed Remanent magnetization of two intrusive bodies in southeastern Finland
title_sort remanent magnetization of two intrusive bodies in southeastern finland
publisher Geological Society of Finland
publishDate 1978
url https://doi.org/10.17741/bgsf/50.1-2.003
https://doaj.org/article/26de9b3fc6674f0b8a7337bcfc48735b
genre Fennoscandia
genre_facet Fennoscandia
op_source Bulletin of the Geological Society of Finland, Vol 50, Iss 1-2, Pp 31-37 (1978)
op_relation http://www.geologinenseura.fi/bulletin/Volume50/sgs_bt_050_pages_031_037.pdf
https://doaj.org/toc/0367-5211
https://doaj.org/toc/1799-4632
doi:10.17741/bgsf/50.1-2.003
0367-5211
1799-4632
https://doaj.org/article/26de9b3fc6674f0b8a7337bcfc48735b
op_doi https://doi.org/10.17741/bgsf/50.1-2.003
container_title Bulletin of the Geological Society of Finland
container_volume 50
container_issue 1-2
container_start_page 31
op_container_end_page 37
_version_ 1765996815405023232

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