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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/21160
Title: Two stages of Late Carboniferous to Triassicmagmatism in the Strandja Zone of Bulgaria and Turkey
Authors: Sałacińska, Anna
Gerdjikov, Ianko
Gumsley, Ashley
Szopa, Krzysztof
Chew, David
Gawęda, Aleksandra
Kocjan, Izabela
Keywords: geochronology; Sakar; Bulgaria; Turkey
Issue Date: 2021
Citation: "Geological Magazine" (Early access) 2021, s. 1-14
Abstract: Although 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.
URI: http://hdl.handle.net/20.500.12128/21160
DOI: 10.1017/S0016756821000650
ISSN: 0016-7568
1469-5081
Appears in Collections:Artykuły (WNP)

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