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.
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