摘要：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.
关键词：Tethys Ocean Closing;Intra Mediterranean Archipelago;New Europe Mosaic Continental Massif;Gondvana\Europe Transcontinental Collision;Quaternary Relief Building
