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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/22281
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dc.contributor.authorJaglarz, Piotr-
dc.contributor.authorRychliński, Tomasz-
dc.contributor.authorFilipiak, Paweł-
dc.contributor.authorUchman, Alfred-
dc.contributor.authorVainorius, Julius-
dc.date.accessioned2022-01-13T10:39:06Z-
dc.date.available2022-01-13T10:39:06Z-
dc.date.issued2021-
dc.identifier.citation"Geological Quarterly", Vol. 65, no. 4, 2021, s. 1-15pl_PL
dc.identifier.issn1641-7291-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/22281-
dc.description.abstractThe Frasnian carbonate-siliciclastic deposits of the Stipinai Formation exposed in two quarries at Petrašiūnai and Klovainiai (northern Lithuania) show considerable vertical facies changes. The lower part of this succession is dominated by argillaceous dolomitic facies with subordinate fine siliciclastic deposits. They display haloturbation and bioturbation structures, represent a hypersaline lagoonal environment, and record the beginning of the transgression. The middle part of the succession consists of secondary dolostones containing moulds of brachiopods, tetracorals, stromatoporoids and trace fossils of deposit feeders; these were deposited in a shallow subtidal marine environment and represent the deepest sedimentary environment of this succession. This was followed by a lagoonal environment (episodic hypersaline), represented by dolomudstones and marly dolomudstones. The upper part of the succession is built of bedded dolostones which document a shallowing trend. Intercalations of clays and palaeosol horizons record emergence events. Palynostratigraphic data tentatively indicate that the Stipinai Formation represents the Upper Frasnian. The succession can be interpreted as a record of the upper part of a T-R cycle (related to the semichatovae transgression) in the Main Devonian Field of the East European Platform. The Stipinai Formation is distributed across western and central Latvia and has a correlative in the Pomerania Basin (northern Poland).pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/pl/*
dc.subjectfaciespl_PL
dc.subjectdolostonespl_PL
dc.subjectrelative sea-level changespl_PL
dc.subjectpalynostratigraphypl_PL
dc.subjectBaltic Basinpl_PL
dc.subjectUpper Devonianpl_PL
dc.titleSedimentary environments and stratigraphy of the Stipinai Formation (Upper Frasnian, northern Lithuania) : a sedimentary record of sea-level changes in the Main Devonian Field of the East European Platformpl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.identifier.doi10.7306/gq.1621-
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