Abstract The Miocene-Pliocene Pannonian Lake formed in an extensional basin system
behind the compressional arc of the Carpathians. Its size and depth were comparable to …

The origin, depositional environment and maturity of petroleum source rocks were
determined via conventional whole rock and biomarker analysis of samples from wells in the …

Lake Pannon was a large lake at the southern margin of the European plate, which
separated from the Central Paratethys at the Sarmatian–Pannonian boundary and was filled …

Detailed sedimentological, facies and numerical cycle analysis, combined with
magnetostratigraphy, have been made in a number of boreholes in the Pannonian Basin, in …

Following an extended biostratigraphical and environmental study of Gastropoda,
Pelecypoda, Ostracoda, Otoliths and other fish remains of the Neogene Kılıç and Yalakdere …

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) …

Considerable volumes of oil and gas in the Pannonian basin have been discovered in
Pliocene sediments having good reservoir characteristics. The Pliocene sediments …

Neogene sedimentany, strata in Hungary contain important mineral resourcs: pelitic rocks,
deposited during the last major deltaic depositional cycle in the Pannonian Basin. are …

A Miocene section of 2 km thickness was continuously cored near Szombathely, NW
Hungary. A detailed magnetostratigraphic study has been integrated with results of …

The evolution and development of the greatest rivers in the Pannonian Basin have been
investigated for almost 150 years. At the end of the Late Miocene Sub-Epoch (7.5-5.3 Ma …