Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region
The Transscandinavian Igneous Belt (TIB) is a major magmatic complex along the western margin of the Svecofennian Domain in the Fennoscandian Shield in which several granitoid generations (TIB 0, TIB 1, TIB 2 and TIB 3) have been recognized (Larson & Berglund 1992). Recent studies have also iden...
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Geological Survey of Finland
2018
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ftunivturku:oai:www.utupub.fi:10024/160527 2023-05-15T16:13:05+02:00 Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region 4th Finnish National Colloquium of Geosciences Turku, 14–15 March 2018: Abstract Book Salin Evgenia Sundblad Krister geologia, Geology 2606902 2018-03-14T00:00:00 https://www.utupub.fi/handle/10024/160527 http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_101.pdf en eng Geological Survey of Finland Espoo Abstract Book 4th Finnish National Colloquium of Geosciences Turku, 14–15 March 2018 4th Finnish National Colloquium of Geosciences https://www.utupub.fi/handle/10024/160527 http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_101.pdf URN:NBN:fi-fe2021042718834 2018 ftunivturku 2022-11-03T00:00:05Z The Transscandinavian Igneous Belt (TIB) is a major magmatic complex along the western margin of the Svecofennian Domain in the Fennoscandian Shield in which several granitoid generations (TIB 0, TIB 1, TIB 2 and TIB 3) have been recognized (Larson & Berglund 1992). Recent studies have also identified the presence of the 1.77–1.81 Ga TIB 1 generation at several drill sites below the Phanerozoic sedimentary cover in the Baltic Sea region: Kvarne on southernmost Gotland (Sundblad et al. 2003), Böda Hamn and Valsnäs on northern and central Öland, respectively (Salin et al. 2018), as well as E-7, offshore on the Latvian/ Lithuanian border (Salin et al. 2016). In this study, we report U–Pb zircon ages from the Precambrian basement in the Baltic Sea region at two more sites: percussion drilling material from Frigsarve (southern Gotland) and drill core D1-1 from the Lithuanian offshore region. Zircons from Frigsarve yielded a LA-ICP-MS age of 1845 ± 4 Ma, which is comparable with the age of the TIB 0 generation in southeastern Sweden. According to crystal morphology and SIMS ages, the zircons from the D1-1 drill core belong to two generations. The larger zircon grains have an age of 1792 ± 8 Ma, which is similar to the TIB 1 generation. The smaller zircon grains are 1744 ± 7 Ma old and are interpreted to record a later 1.73–.68 Ga high-grade metamorphic event, which is widespread in Western Lithuania (Skridlaite et al. 2014). In conclusion, all data from previous and current studies show that the Transscandinavian Igneous Belt extends over vast areas in the Baltic Sea region, from Öand and southern Gotland to the offshore regions of Latvia and Lithuania. Other/Unknown Material Fennoscandian University of Turku: UTUPub Berglund ENVELOPE(17.557,17.557,69.032,69.032) Hamn ENVELOPE(13.415,13.415,66.689,66.689) |
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University of Turku: UTUPub |
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ftunivturku |
language |
English |
description |
The Transscandinavian Igneous Belt (TIB) is a major magmatic complex along the western margin of the Svecofennian Domain in the Fennoscandian Shield in which several granitoid generations (TIB 0, TIB 1, TIB 2 and TIB 3) have been recognized (Larson & Berglund 1992). Recent studies have also identified the presence of the 1.77–1.81 Ga TIB 1 generation at several drill sites below the Phanerozoic sedimentary cover in the Baltic Sea region: Kvarne on southernmost Gotland (Sundblad et al. 2003), Böda Hamn and Valsnäs on northern and central Öland, respectively (Salin et al. 2018), as well as E-7, offshore on the Latvian/ Lithuanian border (Salin et al. 2016). In this study, we report U–Pb zircon ages from the Precambrian basement in the Baltic Sea region at two more sites: percussion drilling material from Frigsarve (southern Gotland) and drill core D1-1 from the Lithuanian offshore region. Zircons from Frigsarve yielded a LA-ICP-MS age of 1845 ± 4 Ma, which is comparable with the age of the TIB 0 generation in southeastern Sweden. According to crystal morphology and SIMS ages, the zircons from the D1-1 drill core belong to two generations. The larger zircon grains have an age of 1792 ± 8 Ma, which is similar to the TIB 1 generation. The smaller zircon grains are 1744 ± 7 Ma old and are interpreted to record a later 1.73–.68 Ga high-grade metamorphic event, which is widespread in Western Lithuania (Skridlaite et al. 2014). In conclusion, all data from previous and current studies show that the Transscandinavian Igneous Belt extends over vast areas in the Baltic Sea region, from Öand and southern Gotland to the offshore regions of Latvia and Lithuania. |
author2 |
geologia, Geology 2606902 |
author |
Salin Evgenia Sundblad Krister |
spellingShingle |
Salin Evgenia Sundblad Krister Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
author_facet |
Salin Evgenia Sundblad Krister |
author_sort |
Salin Evgenia |
title |
Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
title_short |
Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
title_full |
Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
title_fullStr |
Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
title_full_unstemmed |
Distribution of the Transscadinavian Igneous Belt in the Baltic Sea region |
title_sort |
distribution of the transscadinavian igneous belt in the baltic sea region |
publisher |
Geological Survey of Finland |
publishDate |
2018 |
url |
https://www.utupub.fi/handle/10024/160527 http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_101.pdf |
long_lat |
ENVELOPE(17.557,17.557,69.032,69.032) ENVELOPE(13.415,13.415,66.689,66.689) |
geographic |
Berglund Hamn |
geographic_facet |
Berglund Hamn |
genre |
Fennoscandian |
genre_facet |
Fennoscandian |
op_relation |
Abstract Book 4th Finnish National Colloquium of Geosciences Turku, 14–15 March 2018 4th Finnish National Colloquium of Geosciences https://www.utupub.fi/handle/10024/160527 http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_101.pdf URN:NBN:fi-fe2021042718834 |
_version_ |
1765998688920928256 |