Gravity-flow dominated sedimentation on the Buda paleoslope (Hungary): Record of Late Eocene continental escape of the Bakony unit-Reference-Cited by-同舟云学术

Gravity-flow dominated sedimentation on the Buda paleoslope (Hungary): Record of Late Eocene continental escape of the Bakony unit

Published:1992-10 Issue:3 Volume:81 Page:695-716
ISSN:0016-7835
Container-title:Geologische Rundschau
language:en
Short-container-title:Geol Rundsch

Author:

Fodor L.,Magyari A.,Kázmér M.,Fogarasi A.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/BF01791386.pdf

Reference68 articles.

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2. Báldi, T. (1982): Mid-Tertiary tectonic and palaeogeographic evolution of the Carpathian-East Alpine-Pannonian system.- Öslénytani Viták (Discussiones Palaeontologicae),28, 79–155, Budapest. (In Hungarian with English abstract).

3. — (1986): Mid-Tertiary Stratigraphy and Paleogeographic Evolution of Hungary. - Akadémiai Kiadó, Budapest, 201 pp.

4. — &Báldi-Beke, M. (1985): The evolution of the Hungarian Paleogene basins.- Acta Geol. Hungarica,28, 5–28, Budapest.

5. —,Horváth, M., Nagymarosy, A. &Varga, P. (1984): The Eocene-Oligocene boundary in Hungary. The Kiscellian Stage. - Acta Geol. Hungarica,27, 41–65, Budapest.

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