Are There Olistoliths on the Eperkés Hill? The Paleomagnetic Answer

摘要

An abstract of a study by Convert, Marton and Haas exploring the Eperkes Hill to find olistoliths is presented. The results confirm that large blocks of late Triassic-Early Jurassic limestones were moved and re-deposited during the Late Jurassic-Early Cretaceous in the Transdanubian Range, therefore the geodynamic conditions must have been the same as in the Northern Calcareous Alps.