Peri-Amazonian provenance of the Euxinic Craton components in Dobrogea and of the North Dobrogean Orogen components (Romania): A detrital zircon study

Peri-Amazonian provenance of the Euxinic Craton components in Dobrogea and of the North Dobrogean... 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 http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Precambrian Research Elsevier

Peri-Amazonian provenance of the Euxinic Craton components in Dobrogea and of the North Dobrogean Orogen components (Romania): A detrital zircon study

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Publisher
Elsevier
Copyright
Copyright © 2016 Elsevier B.V.
ISSN
0301-9268
eISSN
1872-7433
D.O.I.
10.1016/j.precamres.2016.03.008
Publisher site
See Article on Publisher Site

Abstract

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

Journal

Precambrian ResearchElsevier

Published: Jun 1, 2016

References

  • Avalonian and Cadomian terranes in North Dobrogea, Romania
    Balintoni, I.; Balica, C.; Seghedi, A.; Ducea, M.N.
  • Growth of continental crust: a balance between preservation and recycling
    Condie, K.C.
  • Episodic zircon age spectra of orogenic granitoids: the supercontinent connection and continental growth
    Condie, K.C.; Aster, R.C.
  • Detrital zircon U-Pb geochronology applied to tectonics
    Gehrels, G.
  • Enhanced precision, accuracy, efficiency, and spatial resolution of U–Pb ages by laser ablation–multicollector–inductively coupled plasma–mass spectrometry
    Gehrels, G.E.; Valencia, V.; Ruiz, J.
  • Evolution of the African continental crust as recorded by U–Pb, Lu–Hf and O isotopes in detrital zircons from modern rivers
    Iizuka, T.; Campbell, I.H.; Allen, C.M.; Gill, J.B.; Maruyama, S.; Makoka, F.
  • Assembly, configuration, and break-up history of Rodinia: a synthesis
    Li, Z.X.; Bogdanova, S.V.; Collins, A.S.; Davidson, A.; De Waele, B.; Ernst, R.E.; Fitzsimons, I.C.W.; Fuck, R.A.; Gladkochub, D.P.; Jacobs, J.; Karlstrom, K.E.; Lu, S.; Natapov, L.M.; Pease, V.; Pisarevsky, S.A.; Thrane, K.; Vernikovsky, V.
  • Reliability and longitudinal change of detrital-zircon age spectra in the Snake River system, Idaho and Wyoming: an example of reproducing the bumpy barcode
    Link, P.K.; Fanning, C.M.; Benarek, L.P.
  • On the visualisation of detrital age distributions
    Vermeesch, P.

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