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Krastev (2011)
Sv Stankova Natural Geography of Bulgaria and Sea Part II Regional Characteristic Natural Areas ISBN
(2015)
Geomorphology and morphogenesis of water catchment basin Suha reka river
Tzankov
Sv and principal regional units of the Bulgarian Continental Micro Part of Balkan PeninsulaEast Acta
(2011)
The Morphostructure of the East Stara Planina, С., “Grafika
Tzankov
Sv About the origin and morphostructure of the Black Sea Basin Proceedings of the XIII Conference Natural ISBNSciences
(2003)
Т.Krastev. Geomorphology, construction and development of the Dvoinica
(2014)
, Sv . Stankova . Borders and principal regional units of the Bulgarian Continental Micro Morphotecture ( East Part of Balkan Peninsula )
(2015)
Geomorphology, construction and development of the Durankulak and Shabla-Ezerets limans
Stankova
Sv and morphogenesis of water catchment basin Suha reka river Proceedings of the XIII Conference Natural ISBNGeomorphology Sciences
(2014)
Borders and principal regional units of the Bulgarian Continental Micro Morphotecture (East Part of Balkan Peninsula)
(2011)
Natural Geography of Bulgaria and Black Sea. Part II – Regional Characteristic – Natural Areas, C. “Faber
Tzankov (2017)
Sv of the Mountains ISSN https orgActa Online, 9
Tzankov (2011)
Sv The of the ISBNEast, 19
Stankova (2004)
Sv construction and development of the Fandakliiska Problems of theGeomorphology Geography
(2015)
About the origin and morphostructure of the Black Sea Basin
T. Tzankov, S. Stankova, Rosen Iliev (2017)
Morphostructure of the Sakar and Strandzha MountainsActa Scientifica Naturalis, 4
Stankova (2003)
Sv construction and development of the Proceedings of the Anniversary Conference Years University of vol NaturalGeomorphology Sciences Geography, 30
AbstractThe Black Sea Neozoic passive continental margin marks the natural „bridge” between the Moesian and Bulgarian continental microplates and the Black Sea oceanic microplatte. It was coming in to being after the saturation between the terrains which are composed the Neo Europe south east part during the Early Paleogene. The subaerial part of the margin includes the most east parts of the South Moesian, Hemus, and Upper Thracian and Sakar-Strandzha morphostructural zones. The subaquatic part of the margin is composed by the consequently orderly step lower to the Black Sea bottom: high shelf zone, lover shelf zone, continental slope and continental foot. The Black Sea Neozoic passive continental margin is characterized by low seismic activity. It is concentrated in some fault zones.
Acta Scientifica Naturalis – de Gruyter
Published: Mar 1, 2018
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