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The term Carpathian Basin is used in Hungarian literature, while the West Slavic languages (Czech, Polish and Slovak), the Serbo-Croatian, German and Romanian languages use Pannonian Basin (in Hungarian the basin is known as Kárpát-medence, in Czech; Panonská pánev, in Polish; PanoĊski Basen, in Slovak; Panónska panva, in Slovenian and ...
Mapping increased after the war, with a growing staff at the Geological Survey and a new map was released in 1956. Understanding of Hungarian geology changed with the introduction of plate tectonics theories in the 1970s, which changed views on the formation of the Pannonian Basin. [citation needed]
The Pannonian Region is a large alluvial basin surrounded by the Carpathian Mountains to the north and east, the Alps to the west and the Dinaric Alps to the south. The basin was once the bed of an inland sea. It is flat, and is crossed from north to south by the Danube and Tisza rivers. The region contains all of Hungary, and around the ...
The geology of Croatia has some Precambrian rocks mostly covered by younger sedimentary rocks and deformed or superimposed by tectonic activity. [1] The country is split into two main onshore provinces, a smaller part of the Pannonian Basin and the larger Dinarides. These areas are very different.
The Jurassic-Cretaceous tectonic structure was later changed by various types of the overstep complexes: the Central Carpathian Paleogene Basin, Buda Paleogene Basin, Vienna Basin (Neogene, pull-apart type), Pannonian Basin (or the Danube Basin), and the volcanic complexes: Neogene volcanics of Carpathians (or just Neovolcanis). [12]
Pelso and Tisza units, the Zágráb-Hornád line is the former plate margin between them. Pelso plate or Pelsonia Terrane is a small tectonic unit. It is situated in the Pannonian Basin in Europe.
Pelso and Tisza units. The Tisza plate is a tectonic block, or microplate, in present-day Europe.The two major crustal blocks of the Pannonian Basin, Pelso and Tisza, underwent a complex process of rotation and extension of variable magnitude during the Cenozoic era.
Bulk of the lowlands are found in the northern regions of the country, especially in Slavonia, representing a part of the Pannonian Basin. Territory with elevations of 200 to 500 metres (660 to 1,640 feet) above sea level encompasses 25.61% of Croatia's territory, and the areas between 500 and 1,000 metres (1,600 and 3,300 feet) above sea level ...