Alluvial Architecture and Fluvial Cycles in Quaternary Deposits in a Continental Interior Basin, E Hungary
The thickness of the studied Quaternary alluvial complex, locatedin the eastern part of the Pannonian Basin System, can exceed500 m.Based on subsurface facies analysis the following large-scaledepositional elements were identified: channel-fill deposits, point bardeposits, alluvial fan (sandy sheet-flood) deposits, floodplain andfloodbasin deposits