Geology and History of Evolution of the ALCAPA Mega-Unit
作者： Tibor Szederkényi , Sándor Kovács , János Haas , András Nagymarosy
DOI: 10.1007/978-3-642-21910-8_1
关键词: Stratigraphy 、 Prospecting 、 Carbonate platform 、 Croatian 、 Lineament 、 Archaeology 、 Basement (geology) 、 Pannonian basin 、 Geomorphology 、 Terrane 、 Geology
摘要: The Tisza Mega-unit (Tisia Terrane) forms the basement of Pannonian Basin south Mid-Hungarian Lineament (see Fig. 1 in “Introduction”). In territory Hungary pre-Neogene crops out only two relatively small, isolated areas South Transdanubia – Mecsek Mountains and Villany Hills (Figs. 1, 2 However, more than three thousand wells, oil uranium prospecting boreholes provide information on geologic features younger overburden basins. Significant parts extend into Croatian (Slavonian), Serbian (North Vojvodina) Romanian (West Transylvanian) territories (Szederkenyi 1974, 1984; Kovacs 1982; Fulop 1994; et al. 2000). Romania Croatia large mountains uplands (Apuseni Mts., Papuk Psunj Mts.) an excellent opportunity to study its structural setting stratigraphy.
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