Implications for the Kinematic Evolution of the Carpathian and Aegean Arcs
Earth and Planetary Science Letters 273 (2008) 345–358 Contents lists available at ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl No significant post-Eocene rotation of the Moesian Platform and Rhodope (Bulgaria): Implications for the kinematic evolution of the Carpathian and Aegean arcs Douwe J.J. van Hinsbergen a,⁎, Guillaume Dupont-Nivet a, Radoslav Nakov b, Karen Oud a, Christian Panaiotu c a Paleomagnetic Laboratory ‘Fort Hoofddijk’, Utrecht University, Budapestlaan 17, 3584 CD Utrecht, The Netherlands b Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev St., Bl. 24, 1113 Sofia, Bulgaria c University of Bucharest, Paleomagnetic Laboratory, Balcescu 1, Bucharest, Romania article info abstract Article history: The region located between the Carpathian–Balkan and Aegean arcs, the Moesian Platform and Bulgarian Received 25 February 2008 Rhodope, is generally assumed to have been stably attached to the East European craton during the Cenozoic Received in revised form 26 June 2008 evolution of these arcs. The kinematic evolution of this region is, however, poorly constrained by paleomagnetic Accepted 29 June 2008 analysis. In this paper we provide new paleomagnetic data (800 volcanic and sedimentary samples from 12 Available online 15 July 2008 localities) showing no significant post-Eocene rotation of the Moesian platform and Rhodope with respect to Editor: C.P. Jaupart Eurasia, therefore confirming the stability of this region. We compare this result to a provided review of paleomagnetic data from the South Carpathians (Tisza block) and the Aegean region. The Tisza block underwent Keywords: 68.4±16.7° of middle Miocene (∼15–10 Ma) clockwise rotation with respect to the Moesian Platform, in line with Paleomagnetism previous rotation estimates based on structural geology.
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