Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts

We used LA-ICP-MS U-Pb data for detrital zircon to constrain the Maximum Depositional Age (MDA) and provenance of clastic sedimentary rocks of the Volyn-Orsha sedimentary basin, which filled an elongated (~625 × 250 km) depression in SW Baltica and attained ~900 m in thickness. Eighty-six zircons ou...

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Main Authors: Leonid Shumlyanskyy, Andrey Bekker, Iryna Tarasko, Ion Francovschi, Simon A. Wilde, Viktor Melnychuk
Format: Article
Language:English
Published: MDPI AG 2023-05-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/13/5/152
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author Leonid Shumlyanskyy
Andrey Bekker
Iryna Tarasko
Ion Francovschi
Simon A. Wilde
Viktor Melnychuk
author_facet Leonid Shumlyanskyy
Andrey Bekker
Iryna Tarasko
Ion Francovschi
Simon A. Wilde
Viktor Melnychuk
author_sort Leonid Shumlyanskyy
collection DOAJ
description We used LA-ICP-MS U-Pb data for detrital zircon to constrain the Maximum Depositional Age (MDA) and provenance of clastic sedimentary rocks of the Volyn-Orsha sedimentary basin, which filled an elongated (~625 × 250 km) depression in SW Baltica and attained ~900 m in thickness. Eighty-six zircons out of one hundred and three yielded concordant dates, with most of them (86%) falling in the time interval between 1655 ± 3 and 1044 ± 16 Ma and clustering in two peaks at ca. 1630 and 1230 Ma. The remaining zircons yielded dates older than 1800 Ma. The MDA is defined by a tight group of three zircons with a weighted mean age of 1079 ± 8 Ma. This age corresponds to the time of a ~90° clockwise rotation of Baltica and the formation of the Grenvillian—Sveconorwegian—Sunsas orogenic belts. Subsidence was facilitated by the presence of eclogites derived from subducted oceanic crust. The sediments of the Orsha sub-basin in the northeastern part of the basin were derived from the local crystalline basement, whereas the sediments in the Volyn sub-basin, extending to the margin of Baltica, were transported from the orogen between Laurentia, Baltica and Amazonia.
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spelling doaj.art-30c20f1f85c142ff81d211e0ef28daa32023-11-18T01:31:11ZengMDPI AGGeosciences2076-32632023-05-0113515210.3390/geosciences13050152Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic BeltsLeonid Shumlyanskyy0Andrey Bekker1Iryna Tarasko2Ion Francovschi3Simon A. Wilde4Viktor Melnychuk5School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, AustraliaDepartment of Earth & Planetary Sciences, University of California, Riverside, CA 92521, USARivne Complex Geological Enterprise of the State Ukrainian Geological Company, Stelmakha 11, 33000 Rivne, UkraineFaculty of Geology and Geophysics, University of Bucharest, 010041 Bucharest, RomaniaSchool of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, AustraliaInstitute of Water and Environmental Engineering, National University of Water and Environmental Engineering, 33028 Rivne, UkraineWe used LA-ICP-MS U-Pb data for detrital zircon to constrain the Maximum Depositional Age (MDA) and provenance of clastic sedimentary rocks of the Volyn-Orsha sedimentary basin, which filled an elongated (~625 × 250 km) depression in SW Baltica and attained ~900 m in thickness. Eighty-six zircons out of one hundred and three yielded concordant dates, with most of them (86%) falling in the time interval between 1655 ± 3 and 1044 ± 16 Ma and clustering in two peaks at ca. 1630 and 1230 Ma. The remaining zircons yielded dates older than 1800 Ma. The MDA is defined by a tight group of three zircons with a weighted mean age of 1079 ± 8 Ma. This age corresponds to the time of a ~90° clockwise rotation of Baltica and the formation of the Grenvillian—Sveconorwegian—Sunsas orogenic belts. Subsidence was facilitated by the presence of eclogites derived from subducted oceanic crust. The sediments of the Orsha sub-basin in the northeastern part of the basin were derived from the local crystalline basement, whereas the sediments in the Volyn sub-basin, extending to the margin of Baltica, were transported from the orogen between Laurentia, Baltica and Amazonia.https://www.mdpi.com/2076-3263/13/5/152MesoproterozoicNeoproterozoicBalticaAmazoniadetrital zirconVolyn-Orsha basin
spellingShingle Leonid Shumlyanskyy
Andrey Bekker
Iryna Tarasko
Ion Francovschi
Simon A. Wilde
Viktor Melnychuk
Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
Geosciences
Mesoproterozoic
Neoproterozoic
Baltica
Amazonia
detrital zircon
Volyn-Orsha basin
title Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
title_full Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
title_fullStr Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
title_full_unstemmed Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
title_short Detrital Zircon Geochronology of the Volyn-Orsha Sedimentary Basin in Western Ukraine: Implications for the Meso-Neoproterozoic History of Baltica and Possible Link to Amazonia and the Grenvillian—Sveconorwegian—Sunsas Orogenic Belts
title_sort detrital zircon geochronology of the volyn orsha sedimentary basin in western ukraine implications for the meso neoproterozoic history of baltica and possible link to amazonia and the grenvillian sveconorwegian sunsas orogenic belts
topic Mesoproterozoic
Neoproterozoic
Baltica
Amazonia
detrital zircon
Volyn-Orsha basin
url https://www.mdpi.com/2076-3263/13/5/152
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