Origin of red clays around Miskolc (North Hungary)

During the geological mapping of the northern foreland of the Biikk Mountains red clay occurrences were identified by the Department of Mineralogy and Geology, University of Debrecen. Red clays are underlain by Triassic limestone and Miocene, mainly Sarmatian siliciclastic sediments containing tuffa...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Vincze László
Kozák Miklós
Kovács-Pálffy Péter
Papp István
Püspöki Zoltán
Dokumentumtípus: Cikk
Megjelent: Department of Mineralogy, Geochemistry and Petrology, University of Szeged Szeged 2005
Sorozat:Acta mineralogica-petrographica 46
Kulcsszavak:Földtan, Ásványtan, Kőzettan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/25137

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