<abstract xmlns="http://www.w3.org/1999/xhtml"><p>The East Balkan Peninsula Area was a part from the Tethys Ocean until 72 000 000 years. The pre Maestrichtian geologic-tectonic pattern of cockle of the East Balkan Peninsula Area wasn’t built on the Europe Continental Massif. The modern East Balkan Peninsula Relief is forming during the Late Quaternary time. The East Balkan Peninsula Margin coincides with the border between the Bulgarian and Moesian Continental Microplates from the west and the Black Sea Oceanic Microplatte to the east. This border present the Neo Europe West Passive Continental Margin in the area of the last Tethys Oceanic Fragment – it Black Sea Oceanic Gulf.</p></abstract>

The East Balkan Peninsula Area was a part from the Tethys Ocean until 72 000 000 years. The pre Maestrichtian geologic-tectonic pattern of cockle of the East Balkan Peninsula Area wasn’t built on the Europe Continental Massif. The modern East Balkan Peninsula Relief is forming during the Late Quaternary time. The East Balkan Peninsula Margin coincides with the border between the Bulgarian and Moesian Continental Microplates from the west and the Black Sea Oceanic Microplatte to the east. This border present the Neo Europe West Passive Continental Margin in the area of the last Tethys Oceanic Fragment – it Black Sea Oceanic Gulf.

Investigations of the late Quaternary morphotectonic evolution of the Balkan Peninsula East Part

Konstantin Preslavski University of Shumen

Faculty of Natural Sciences, Department of Geography and Regional Development

South-West University „Neofit Rilski“ – Blagoevgrad

Faculty of Mathematics and Natural Sciences, Department of Geography, Ecology and Environment Protection

Acta Scientifica Naturalis

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

The East Balkan Peninsula Area was a part from the Tethys Ocean until 72 000 000 years. The pre Maestrichtian geologic-tectonic pattern of cockle of the East...

Investigations of the late Quaternary morphotectonic evolution of the Balkan Peninsula East Part

Publié en ligne: 10 août 2020

Pages: 122 - 132

DOI: https://doi.org/10.2478/asn-2020-0024

Mots clés
continental fragment, New Europe, Late Quaternary relief

© 2020 Tzanko Tzankov et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

Investigations of the late Quaternary morphotectonic evolution of the Balkan Peninsula East Part

Publié en ligne: 10 août 2020

Pages: 122 - 132

DOI: https://doi.org/10.2478/asn-2020-0024

Mots cléscontinental fragment, New Europe, Late Quaternary relief

© 2020 Tzanko Tzankov et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

Mots clés
continental fragment, New Europe, Late Quaternary relief