Vulkanoklastika v pavlovickém souvrství ždánické jednotky

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Title in English	Volcaniclastics rocks within the deposits of the Pavlovice Formation
Authors	NEHYBA Slavomír STRÁNÍK Zdeněk
Year of publication	2005
Type	Article in Periodical
Magazine / Source	Geologické výzkumy na Moravě a ve Slezsku v roce 2004
MU Faculty or unit	Faculty of Science
Citation
Field	Geology and mineralogy
Keywords	Outer Carapthian Flysch Belt; Neogene; tephrostratigraphy; acidic calc-alcaline source volcanism; distal fallout tephra
Description	Tephrostratigraphical study of volcaniclastics rocks within the deposits of Pavlovice Formation (?Eggenburgian- Karpatian) proved that they represent distal fallout tephra. The studies of volcanic glass, volcanic zircon and geochemistry of the bulk rock (trace elements, REE) revealed that the parental volcanism was acidic calc-alcaline one of the volcanic arch. Studied volcaniclastics are strongly altered.
Related projects:	Depositional archtecture of the Lower Badenian deposits in the southern and middle part of the carpathian Foredeep in Moravia