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Chapter
Correlation of Seismo- and Magnetostratigraphy in Southeastern Hungary
Correlation of results from magnetostratigraphic and seismic-reflection studies indicate that the Pannonian Basin, during the postrift phase of its evolution (middle Miocene to present), became filled by sedim...
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Chapter
Structural Control on Hydrocarbon Accumulation in the Pannonian Basin, Hungary
The Pannonian Basin is a back-arc basin superimposed on the Alpine compressional megasuture that resulted from continental collision between Europe and smaller continental fragments following southward subduct...
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Chapter
Structure of the Békés Basin Inferred from Seismic Reflection, Well and Gravity Data
The Békés basin (areal extent 3900 km2) is a northwest-trending, Neogene basin located in southeast Hungary. The basin contains over 6500 m of synrift and postrift sedimentary fill. Middle Miocene synrift deposit...