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Az eszak-magyarorszagi barnakoszentelepek kora



Az eszak-magyarorszagi barnakoszentelepek kora



Foldtani Kozlony 91(2): 143-146



One third of the Hungarian brown coal deposits occur in the Miocene deposits of Ozd and Nograd. These have been formed at the edge of a 130 km long geosyncline. Based on recent explorations in the area, the age of the coal deposits must be reassigned to the Helvetian stage.

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