New LA-ICP-MS U-Pb zircon dating for Strandja granitoids (SE Bulgaria): evidence for two-stage late Variscan magmatism in the internal Balkanides

Authors

PHILIP MACHEV
VALENTIN GANEV
LASLO KLAIN

DOI

10.3906/yer-1407-21

Abstract

The Strandja Massif (Sakar-Strandja Zone) forms an important link between the Balkan Zone (external Balkanides) of Bulgaria, which is commonly correlated with the Variscan orogen in Central Europe, and the Western Pontides of Turkey. The Bulgarian part of the massif is composed of a metamorphic basement (various granite gneisses, paragneisses, and schists) traditionally interpreted as having Precambrian age, Triassic-Jurassic metasedimentary cover, and Upper Cretaceous volcanosedimentary sequences. The basement is intruded by large granitic plutons of Variscan age that are widespread mostly across Turkish territory. New LA-ICP-MS data support the suggestion of Variscan granitoid magmatism in the studied area but do not confirm the presence of Precambrian rocks. Furthermore, two stages of magmatism are determined in relation to the Variscan metamorphism and deformation. The first one (301.9 ± 1.1 Ma) is represented by strongly deformed metagranites and thus is interpreted as syntectonic, while the second one is relatively younger (293.5 ± 1.7 Ma) and postmetamorphic.

Keywords

Strandja, Variscan granitoid magmatism, SE Bulgaria, geochronology

First Page

230

Last Page

248

Recommended Citation

MACHEV, PHILIP; GANEV, VALENTIN; and KLAIN, LASLO (2015) "New LA-ICP-MS U-Pb zircon dating for Strandja granitoids (SE Bulgaria): evidence for two-stage late Variscan magmatism in the internal Balkanides," Turkish Journal of Earth Sciences: Vol. 24: No. 3, Article 2. https://doi.org/10.3906/yer-1407-21
Available at: https://journals.tubitak.gov.tr/earth/vol24/iss3/2