Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland

In the southernmost part of the Svecofennian province in Finland, leucogranites and migmatites stemming from both igneous and sedimentary protoliths reflect the complex magmatic history of the Svecofennian orogeny between 1.89 and 1.82 Ga. Although the migmatites and leucogranites in southernmost Fi...

Full description

Saved in:
Bibliographic Details
Main Authors: Anna Saukko, Kaisa Nikkilä, Olav Eklund, Sören Fröjdö, Markku Väisänen
Format: Article
Language:English
Published: Geological Society of Finland 2025-01-01
Series:Bulletin of the Geological Society of Finland
Subjects:
Online Access:https://www.geologinenseura.fi/sites/geologinenseura.fi/files/pages_from_bulletin_vol96_part_2_2024_101_133_0.pdf
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832589749191180288
author Anna Saukko
Kaisa Nikkilä
Olav Eklund
Sören Fröjdö
Markku Väisänen
author_facet Anna Saukko
Kaisa Nikkilä
Olav Eklund
Sören Fröjdö
Markku Väisänen
author_sort Anna Saukko
collection DOAJ
description In the southernmost part of the Svecofennian province in Finland, leucogranites and migmatites stemming from both igneous and sedimentary protoliths reflect the complex magmatic history of the Svecofennian orogeny between 1.89 and 1.82 Ga. Although the migmatites and leucogranites in southernmost Finland display similar ages as their counterparts elsewhere in the Southern Finland Subprovince, they differ in field appearance and composition. Field and petrographical observations reveal K-feldspar megacrysts of varying sizes in the migmatized early Svecofennian (c. 1.89–1.87 Ga) supracrustal rocks and granitoids. Whole-rock geochemical analyses likewise display anomalously high K-contents in the early Svecofennian granitoids. Zircon U-Pb dating of migmatites and related leucogranites shows that a late Svecofennian partial melting event occurred at 1.84–1.82 Ga, possibly in several pulses. The morphological features of the migmatites as well as neosome mineralogy indicate a formation mechanism different from the dehydration melting prevalent elsewhere in the Subprovince.
format Article
id doaj-art-1affebaa20304f61ae0c82baf55986ad
institution Kabale University
issn 0367-5211
1799-4632
language English
publishDate 2025-01-01
publisher Geological Society of Finland
record_format Article
series Bulletin of the Geological Society of Finland
spelling doaj-art-1affebaa20304f61ae0c82baf55986ad2025-01-24T08:40:52ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46322025-01-0196210113410.17741/bgsf/96.2.001Petrology, geochemistry, and geochronology of the leucogranites in southernmost FinlandAnna Saukko0Kaisa Nikkilä1Olav Eklund2Sören Fröjdö3Markku Väisänen4Geology and Mineralogy, Åbo Akademi University, Turku, Finland Geology and Mineralogy, Åbo Akademi University, Turku, Finland Geology and Mineralogy, Åbo Akademi University, Turku, Finland Geology and Mineralogy, Åbo Akademi University, Turku, Finland Department of Geography and Geology, University of Turku, FinlandIn the southernmost part of the Svecofennian province in Finland, leucogranites and migmatites stemming from both igneous and sedimentary protoliths reflect the complex magmatic history of the Svecofennian orogeny between 1.89 and 1.82 Ga. Although the migmatites and leucogranites in southernmost Finland display similar ages as their counterparts elsewhere in the Southern Finland Subprovince, they differ in field appearance and composition. Field and petrographical observations reveal K-feldspar megacrysts of varying sizes in the migmatized early Svecofennian (c. 1.89–1.87 Ga) supracrustal rocks and granitoids. Whole-rock geochemical analyses likewise display anomalously high K-contents in the early Svecofennian granitoids. Zircon U-Pb dating of migmatites and related leucogranites shows that a late Svecofennian partial melting event occurred at 1.84–1.82 Ga, possibly in several pulses. The morphological features of the migmatites as well as neosome mineralogy indicate a formation mechanism different from the dehydration melting prevalent elsewhere in the Subprovince.https://www.geologinenseura.fi/sites/geologinenseura.fi/files/pages_from_bulletin_vol96_part_2_2024_101_133_0.pdfsvecofenniansouthern finland subprovincemigmatiteleucogranitek-feldspar megacrystzircon u-pbwhole-rock geochemistry
spellingShingle Anna Saukko
Kaisa Nikkilä
Olav Eklund
Sören Fröjdö
Markku Väisänen
Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
Bulletin of the Geological Society of Finland
svecofennian
southern finland subprovince
migmatite
leucogranite
k-feldspar megacryst
zircon u-pb
whole-rock geochemistry
title Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
title_full Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
title_fullStr Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
title_full_unstemmed Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
title_short Petrology, geochemistry, and geochronology of the leucogranites in southernmost Finland
title_sort petrology geochemistry and geochronology of the leucogranites in southernmost finland
topic svecofennian
southern finland subprovince
migmatite
leucogranite
k-feldspar megacryst
zircon u-pb
whole-rock geochemistry
url https://www.geologinenseura.fi/sites/geologinenseura.fi/files/pages_from_bulletin_vol96_part_2_2024_101_133_0.pdf
work_keys_str_mv AT annasaukko petrologygeochemistryandgeochronologyoftheleucogranitesinsouthernmostfinland
AT kaisanikkila petrologygeochemistryandgeochronologyoftheleucogranitesinsouthernmostfinland
AT olaveklund petrologygeochemistryandgeochronologyoftheleucogranitesinsouthernmostfinland
AT sorenfrojdo petrologygeochemistryandgeochronologyoftheleucogranitesinsouthernmostfinland
AT markkuvaisanen petrologygeochemistryandgeochronologyoftheleucogranitesinsouthernmostfinland