Precambrian Research 278 (2016) 34–51 Contents lists available at ScienceDirect Precambrian Research journal homepage: www.elsevier.com/locate/precamres Peri-Amazonian provenance of the Euxinic Craton components in Dobrogea and of the North Dobrogean Orogen components (Romania): A detrital zircon study I. Balintoni, C. Balica Department of Geology, Babes-Bolyai University, 400084 Cluj-Napoca, Romania ar ti c l e i nf o ab stra ct Article history: The Romanian South Carpathians foreland is located southwards of the East European Craton (EEC) and Received 14 May 2015 consists of three major tectonic units: the Scythian Platform, the North Dobrogean Orogen and the Revised 14 October 2015 Euxinic Craton. The Euxinic Craton is represented in the Dobrogea area by two components: (i) Central Accepted 15 March 2016 Dobrogean Shield and (ii) East Moesia. In central-northern Dobrogea, the Trans European Suture Zone Available online 23 March 2016 (TESZ), including the Teisseyre–Tornquist Zone, presumably strikes below the surface. Because the pale- ogeographic provenance of the above tectonic units was poorly documented until present, a systematic Keywords: sampling for detrital zircon has been conducted in all tectonic units except for the Scythian Platform Detrital zircon basement which is entirely covered by the Danube Delta. In all, this totals 26 samples
Precambrian Research – Elsevier
Published: Jun 1, 2016
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