Grain-size analysis of the Neogene red clay formation in the Pannonian Basin

Author:

Kovács János

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference39 articles.

1. Ballenegger R (1917) About the clay soils of the foothills of the Tokaj Mountains (in Hungarian). Földt Közl (Bull Hung Geol Soc) 48:20–24

2. Bárdossy G, Aleva GJJ (1990) Lateritic bauxites. Developments in economic geology, vol 27. Elsevier, Amsterdam, pp 1–624

3. Berényi-Üveges J, Horváth Z, Michéli E, Mindszenty A, Németh T (2003) Reconstructing quaternary pedogenesis in a paleosol sequence in Hungary. Quat Int 106/107:61–71

4. Ding Z, Sun J, Yang S, Liu T (1998) Preliminary magnetostratigraphy of a thick eolian red clay-loess sequence at Lingtai, the Chinese Loess Plateau. Geophys Res Lett 25:1225–1228

5. Fábián SzÁ, Kovács J, Nagyváradi L, Varga G (2004a) Was there desert climate in the Carpathian Basin, or not? Studia Geomorphologica Carpatho Balcanica 38:49–58

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