engleski

Remotwe sensing review of the Pannonian basin S.L. morphostrustural complex

The purpose of this article is to show the remote sensing of the combined Pannonian Basin oval structure tectodynamic influence, developed on the gravimetric maximum and the network of the lineament structures on the narrower and wider border areas in the morphostructural sense. It has been reflected on the formation of the larger polygonal to ringlike masked relief complex named the Pannonian Basin s. l. It integrates in its complex various tectonic units as Dinarides, the parts of the Eastern Alps, Moesian plate, Carpathians range and Rhodopians unit, representing the specific feature of the SE Europian morphostructural evolution. The singled out complex is ranked as the masked trend morphostructure, because it is not directly noticeable by visual observation. In its totality in indirectly indicates the continual tectonic activity of the Earth's crust underground. However, it hasn't developed so much yet, as to disrupt or transform the existing or-tectonic plan which can be identified on the standard geographic and geological maps. In the aforementioned relationship disclosure, the denudational-accumulative processes played also a very important role.

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