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...

Full description

Bibliographic Details
Main Authors: Salin Evgenia, Sundblad Krister
Other Authors: geologia, Geology, 2606902
Language:English
Published: Geological Survey of Finland 2018
Subjects:
Online Access:https://www.utupub.fi/handle/10024/160527
http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_101.pdf
id ftunivturku:oai:www.utupub.fi:10024/160527
record_format openpolar
spelling 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)
institution Open Polar
collection University of Turku: UTUPub
op_collection_id 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