Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon
Zircons from nine Palaeoproterozoic granitoid intrusions within the southern part of the Fennoscandian Shield have been studied by laser ablation inductively coupled plasma source mass spectrometry to obtain U–Pb ages (in the range 1.88–1.68 Ga) and Hf isotope compositions. Six granitoids are from t...
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Geological Society of London
2016
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ftdatacite:10.6084/m9.figshare.3454589.v1 2023-05-15T16:11:43+02:00 Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon Andersen, Tom Andersson, Ulf Bertil Graham, Stuart Åberg, Göran Simonsen, Siri L. 2016 https://dx.doi.org/10.6084/m9.figshare.3454589.v1 https://geolsoc.figshare.com/articles/dataset/Granitic_magmatism_by_melting_of_juvenile_continental_crust_new_constraints_on_the_source_of_Palaeoproterozoic_granitoids___in_Fennoscandia_from_Hf_isotopes_in_zircon/3454589/1 unknown Geological Society of London https://dx.doi.org/10.1144/0016-76492007-166 https://dx.doi.org/10.6084/m9.figshare.3454589 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geology FOS Earth and related environmental sciences dataset Dataset 2016 ftdatacite https://doi.org/10.6084/m9.figshare.3454589.v1 https://doi.org/10.1144/0016-76492007-166 https://doi.org/10.6084/m9.figshare.3454589 2021-11-05T12:55:41Z Zircons from nine Palaeoproterozoic granitoid intrusions within the southern part of the Fennoscandian Shield have been studied by laser ablation inductively coupled plasma source mass spectrometry to obtain U–Pb ages (in the range 1.88–1.68 Ga) and Hf isotope compositions. Six granitoids are from the 1.85–1.65 Ga Transscandinavian Igneous Belt; during that period more than 10 6 km 3 of granitoid magma intruded the pre-existing crust. The large majority of magmatic zircons from the nine granitoids have a limited initial range, 176 Hf/ 177 Hf = 0.2816–0.2818, and define an evolutionary trend given by an initial value of ε Hf(1.88Ga) ≈ +2 ± 3 at an average 176 Lu/ 177 Hf = 0.015. These data show that a geographically extensive, long-lived, relatively homogeneous, and dominant magma source resided within 2.1–1.86 Ga Svecofennian juvenile crust between 1.88 and 1.68 Ga. Zircon xenocrysts (1.91–1.98 Ga) with initial ε Hf = +0 to +2.5 from one of the intrusions provide additional evidence for such a long-lived crustal source of granitic magmas in central Fennoscandia. The granitoids were emplaced during a period of active mafic underplating that supplied heat to the anatectic zone in the lower–middle crust, but little or no mantle-derived Hf to the granitic magmas, in contrast to many mixed intermediate rocks. Dataset Fennoscandia Fennoscandian DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Geology FOS Earth and related environmental sciences |
spellingShingle |
Geology FOS Earth and related environmental sciences Andersen, Tom Andersson, Ulf Bertil Graham, Stuart Åberg, Göran Simonsen, Siri L. Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
topic_facet |
Geology FOS Earth and related environmental sciences |
description |
Zircons from nine Palaeoproterozoic granitoid intrusions within the southern part of the Fennoscandian Shield have been studied by laser ablation inductively coupled plasma source mass spectrometry to obtain U–Pb ages (in the range 1.88–1.68 Ga) and Hf isotope compositions. Six granitoids are from the 1.85–1.65 Ga Transscandinavian Igneous Belt; during that period more than 10 6 km 3 of granitoid magma intruded the pre-existing crust. The large majority of magmatic zircons from the nine granitoids have a limited initial range, 176 Hf/ 177 Hf = 0.2816–0.2818, and define an evolutionary trend given by an initial value of ε Hf(1.88Ga) ≈ +2 ± 3 at an average 176 Lu/ 177 Hf = 0.015. These data show that a geographically extensive, long-lived, relatively homogeneous, and dominant magma source resided within 2.1–1.86 Ga Svecofennian juvenile crust between 1.88 and 1.68 Ga. Zircon xenocrysts (1.91–1.98 Ga) with initial ε Hf = +0 to +2.5 from one of the intrusions provide additional evidence for such a long-lived crustal source of granitic magmas in central Fennoscandia. The granitoids were emplaced during a period of active mafic underplating that supplied heat to the anatectic zone in the lower–middle crust, but little or no mantle-derived Hf to the granitic magmas, in contrast to many mixed intermediate rocks. |
format |
Dataset |
author |
Andersen, Tom Andersson, Ulf Bertil Graham, Stuart Åberg, Göran Simonsen, Siri L. |
author_facet |
Andersen, Tom Andersson, Ulf Bertil Graham, Stuart Åberg, Göran Simonsen, Siri L. |
author_sort |
Andersen, Tom |
title |
Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
title_short |
Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
title_full |
Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
title_fullStr |
Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
title_full_unstemmed |
Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon |
title_sort |
granitic magmatism by melting of juvenile continental crust: new constraints on the source of palaeoproterozoic granitoids in fennoscandia from hf isotopes in zircon |
publisher |
Geological Society of London |
publishDate |
2016 |
url |
https://dx.doi.org/10.6084/m9.figshare.3454589.v1 https://geolsoc.figshare.com/articles/dataset/Granitic_magmatism_by_melting_of_juvenile_continental_crust_new_constraints_on_the_source_of_Palaeoproterozoic_granitoids___in_Fennoscandia_from_Hf_isotopes_in_zircon/3454589/1 |
genre |
Fennoscandia Fennoscandian |
genre_facet |
Fennoscandia Fennoscandian |
op_relation |
https://dx.doi.org/10.1144/0016-76492007-166 https://dx.doi.org/10.6084/m9.figshare.3454589 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.3454589.v1 https://doi.org/10.1144/0016-76492007-166 https://doi.org/10.6084/m9.figshare.3454589 |
_version_ |
1765996892131426304 |