New ideas about the Balkan peninsula East Part morphotectonics

Tzanko Tzankov 1  and Svetla Stankova 2
  • 1 South-West University „Neofit Rilski“ – Blagoevgrad, Faculty of Mathematics and Natural Sciences, Department of Geography, Ecology and Environment Protection, 2700, Blagoevgrad
  • 2 Konstantin Preslavski University of Shumen, Faculty of Natural Sciences, Department of Geography and Regional Development, Shumen 9712, 115 Universitetska Str.,

Abstract

The article introduces the results of the author’s new investigations about the origin, Quaternary morphotectonic evolution and the modern morphostructure of the Bulgarian Continental Microplate in the eastern part of Balkan Peninsula. The research was realized on a base of the contemporary Plate tectonic study principia by means of the morphostructural analysis apply. It was provided the principal relief building role of the regional mosaic pattern and the listric faulting in the Balkan Peninsula East Part.

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  • [1] Tzankov, Tz., General aspects of the Neogene-Quaternary listric tectonics of Bulgaria. In: Global changes, vulnerability, mitigation and adaption. Proceedings of Fifth International conference, 17-18 April 2008, Sofia University „St. Kliment Ohridski”, Faculty of Geology and Geography, „St Kliment Ohridski” University Press, Sofia Bulgaria, 2009, 116-120.

  • [2] Tzankov, Tz., About the contemporary geodynamics of the Balkan peninsula. In: Global changes, vulnerability, mitigation and adaption. Proceedings of Fifth International conference, 17-18 April 2008, Sofia University „St. Kliment Ohridski”, Faculty of Geology and Geography, „St Kliment Ohridski” University Press, Sofia Bulgaria, 2009a, 126-128.

  • [3] Tzankov, Tz., Morphostructural survey of the Bulgarian microplate. Proceedings of International Scientific Conference FMNS’2009, SWU „Neofit Rilski”, Blagoevgrad, 2009b.

  • [4] Tzankov, Tz.; Stankova, Sv., Borders and principal regional units of the Bulgarian Continental Micro Morphotecture (East Part of Balkan Peninsula). Acta Scientifica Naturalis, 2014, 1, 218-232.

  • [5] Tzankov, Tz.; Stankova, Sv., About the origin and morphostructure of the Black Sea Basin. Prosedings of the XIII Conference “Natural Sciences’2015”, September 25-27, 2015,Varna, Bulgaria, University Printing House “Bishop Konstantin Preslavski”, Shumen, 2015, 74-76.

  • [6] Tzankov, Tz.; Stankova, Sv., Post Early Pleistocene Pattern of the South Moesian Morphostructural Zone. Fourth Romanian-Bulgarian-Hungarian-Serbian Conference “Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube”, Vidin, 2016.

  • [7] Tzankov, Tz.; Stankova, Sv.; Iliev, R., Morphostructure of the Sakar and Strandzha Mountains. Acta Scientifica Naturalis, 2017, 4 (1), 94-99, doi: https://doi.org/10.1515/asn-2017-oo14.

  • [8] Tzankov, Tz.; Stankova, Sv.; Iliev, R., Morphostructure of the Rila-Pirin Mountains Range. LAP LAMBERT Academic Publishing. Düsseldorf, Germany, 2017a, p. 64.

  • [9] Tzankov, Tz.; Stankova, Sv.; Iliev, R., Mitkov, I., Survey of the Middle Struma Complex Morphostructural Passage (South-West Bulgaria). Universal Journal of Geoscience, 2017b, 5(6), 191-196, doi: 10.13189/ujg.2017.050604.

  • [10] Tzankov, Tz.; Stankova, Sv.; Iliev, R., Mitkov, I., Late Quaternary morphostructural generations in the eastern part of the Balkan Peninsula. SocioBrains, 2018, 41, 188-197.

  • [11] Tzankov, Tz.; Iliev, R., Morphostructure of the Rhodopean Mountain massif. Printing House „Grafika 19“, Sofia, 2015.

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