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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/21160
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dc.contributor.authorSałacińska, Anna-
dc.contributor.authorGerdjikov, Ianko-
dc.contributor.authorGumsley, Ashley-
dc.contributor.authorSzopa, Krzysztof-
dc.contributor.authorChew, David-
dc.contributor.authorGawęda, Aleksandra-
dc.contributor.authorKocjan, Izabela-
dc.date.accessioned2021-08-25T10:37:47Z-
dc.date.available2021-08-25T10:37:47Z-
dc.date.issued2021-
dc.identifier.citation"Geological Magazine" (Early access) 2021, s. 1-14pl_PL
dc.identifier.issn0016-7568-
dc.identifier.issn1469-5081-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/21160-
dc.description.abstractAlthough Variscan terranes have been documented from the Balkans to the Caucasus, the southeastern portion of the Variscan Belt is not well understood. The Strandja Zone along the border between Bulgaria and Turkey encompasses one such terrane linking the Balkanides and the Pontides. However, the evolution of this terrane, and the Late Carboniferous to Triassic granitoids within it, is poorly resolved. Here we present laser ablation – inductively coupled plasma – mass spectrometry (LA-ICP-MS) U–Pb zircon ages, coupled with petrography and geochemistry from the Izvorovo Pluton within the Sakar Unit (Strandja Zone). This pluton is composed of variably metamorphosed and deformed granites which yield crystallization ages of c. 251–256 Ma. These ages are older than the previously assumed age of the Izvorovo Pluton based on a postulated genetic relationship between the Izvorovo Pluton and Late Jurassic to Early Cretaceous metamorphism. A better understanding of units across the Strandja Zone can now be achieved, revealing two age groups of plutons within it. An extensive magmatic episode occurred c. 312–295 Ma, and a longer-lived episode between c. 275 and 230 Ma. Intrusions associated with both magmatic events were emplaced into pre-Late Carboniferous basement, and were overprinted by Early Alpine metamorphism and deformation. These two stages of magmatism can likely be attributed to changes in tectonic setting in the Strandja Zone. Such a change in tectonic setting is likely related to the collision between Gondwana-derived terranes and Laurussia, followed by either subduction of the Palaeo-Tethys Ocean beneath Laurussia or rifting in the southern margin of Laurussia, with granitoids forming in different tectonic environments.pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/pl/*
dc.subjectgeochronologypl_PL
dc.subjectSakarpl_PL
dc.subjectBulgariapl_PL
dc.subjectTurkeypl_PL
dc.titleTwo stages of Late Carboniferous to Triassicmagmatism in the Strandja Zone of Bulgaria and Turkeypl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.identifier.doi10.1017/S0016756821000650-
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