Genesis and Evolution of the Pannonian Basin

Fractionation of hydrocarbons and NSO-compounds during primary oil migration revealed by high resolution mass spectrometry: Insights from oil trapped in fluid inclusions

“…The complex movement of crustal plates resulted in amalgamation and the Tisza Mega-unit reached its current position during the Palaeogene and Neogene (Csontos et al, 2002). An extensional half-graben formed during the Rhaetian to Hettangian time, and coal-bearing fluvial-deltaic swamp sediments of the Mecsek Coal Formation were deposited (Haas, 2012). In the early Sinemurian, the subsidence of the Mecsek Basin resulted in the deposition of shallow marine sandstones and marls of the Zobákpuszta Sandstone Formation and Vasas Marl Formation, respectively (Raucsik, 2012a(Raucsik, , 2012b.…”

Computation of daily Penman–Monteith reference evapotranspiration in the Carpathian Region and comparison with Thornthwaite estimates

“…1) is enclosed by the Carpathians and the Transylvanian Plateau to the east and north. Over these regions, the Romanian Lowlands and the Subcarpathian depressions beyond the Carpathians (also known as Transcarpathia) are in the focus of PannEx initiative (Matenco and Radivojević, 2012;Haas et al, 2013).…”

Correlating volcanic dynamics and the construction of a submarine volcanogenic apron: An example from the Badenian (Middle Miocene) of North-Eastern Hungary

“…The NAF comprises terrestrial and subaqueous deposits. The terrestrial sequences form most of the volcanic morphologies and deposits of the Matra Volcanic Complex, whereas the subaqueous part of the NAF is exposed in the Nógrád Basin (e.g., Karátson et al, 2001;Póka et al, 2004;Nagymarosy and Hámor, 2013). There, the NAF is intercalated by the transgressive fossiliferous, clastic to calcareous deposits of the Pécsszabolcs Limestone Member (PLM), Early Badenian in age (Fig.…”