Miocene to Quaternary deformation, stratigraphy and paleogeography in Northeastern Slovenia and Southwestern Hungary

Miocene to Quaternary deformation, stratigraphy and paleogeography in Northeastern Slovenia and Southwestern Hungary

The Mura-Zala basin was formed due to ENE-WSW trending crustal extension in the late early and middle Miocene (19 – 11 Ma). Marine sedimentation occurred in several more or less confined depressions (half grabens), then in a unified basin. The rifting phasewas probably connected to uplift and brittl...

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Bibliographic Details
Main Authors: Laszlo Fodor, Bogoljub Jelen, Emo Marton, Helena Rifelj, Marijan Kraljić, Renata Kervić, Peter Marton, Balazs Koroknai, Maria Baldi-Beke
Format: Article
Language:English
Published: Geological Survey of Slovenia 2002-06-01
Series:Geologija
Subjects:
faulting
folding
subsidence
uplift
paleomagnetism
rotation
paleostress
depositional environment
Neogene
Pannonian basin
Slovenia
SW Hungary
Online Access:http://www.geologija-revija.si/dokument.aspx?id=606

Internet

http://www.geologija-revija.si/dokument.aspx?id=606

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