Geology and K-Ar geochronology of illite from the clay deposit at Füzérradvány, Tokaj Mts., Hungary

Illite deposit of Fiizerradvany is a part of a low sulphidation type epithermal system hosted by an Upper Miocene (Sarmatian) volcanoclastic and sedimentary sequence. Mineable high quality illite bodies were formed along siliceous veins due to interaction of hydrothermal fluids with permeable rock u...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Pécskay Zoltán
Molnár Ferenc
Itaya Tetsumaru
Zelenka Tibor
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/25135

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