Abstract
The ALCAPA Mega-unit (composite terrane) consists of elements of the Austroalpine and Penninic Units (Eastern Alps), the Central and Inner Western Carpathian Units, and the Pelso Composite Unit (northwestern part of the basement of the Pannonian Basin, see Fig. 1.1), which were amalgamated during the Palaeogene to Early Miocene. The name ALCAPA, proposed by Csontos et al. (1992), is derived from the names ALps, CArpathians, and PAnnonian Basin.
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References
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Szederkényi, T., Kovács, S., Haas, J., Nagymarosy, A. (2012). Geology and History of Evolution of the ALCAPA Mega-Unit. In: Haas, J. (eds) Geology of Hungary. Regional Geology Reviews. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-21910-8_1
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