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- W2021874170 abstract "The geological and geochronological relationships between a rhyolite, belonging to the Transscandinavian Igneous Belt (TIB), and an intrusive suite (the Bäckaby intrusion), southeast Sweden, have been investigated by means of bedrock mapping, geochemistry and radiometric age determinations (UPb on zircons). Field relations suggest that the rhyolite rests unconformably on the Bäckaby intrusion, which previously has been correlated with ∼ 1.9 Ga granitoids within the Svecofennian Domain. The rhyolite yielded an age of 1800 ± 8 Ma and a tonalite belonging to the Bäckaby intrusion basement yielded an age of 1834 ± 3 Ma. The age of the rhyolite is slightly older (10–15 Ma) than adjacent granitoids belonging to the Transscandinavian Igneous Belt, and is considered as the earliest magmatic expression of TIB in the area. The age and the geochemical trends for the Bäckaby intrusion is significantly different from that of the surrounding TIB granitoids and indicate a rock forming event at about 1830–1840 Ma in southeastern Sweden represented by the Oskarshamn-Jönköping Belt. This event is significantly younger than the older Svecofennian rocks within the Svecofennian Domain proper, indicating a hitherto unidentified geological terrane in southeastern Sweden." @default.
- W2021874170 created "2016-06-24" @default.
- W2021874170 creator A5072919009 @default.
- W2021874170 date "1996-03-01" @default.
- W2021874170 modified "2023-10-16" @default.
- W2021874170 title "Geological, geochemical and geochronological evidence for a new palaeoproterozoic terrane in southeastern Sweden" @default.
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- W2021874170 doi "https://doi.org/10.1016/0301-9268(95)00046-1" @default.
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