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The Sedimentological Significance and Stratigraphic Position of Coarse-Grained Red Beds (?Oligocene) of the Northwestern Margin of Mt. Pozeska Gora (North Croatia)

J. Halamić
M. Belak
D. Pavelić


Puni tekst: engleski pdf 4.538 Kb

str. 137-143

preuzimanja: 673

citiraj


Sažetak

Coarse-grained clastic sediments of rhyolitic-granitic composition which are associated with the magmatic complex of Mt. Pozeska Gora were previously designated as granites. They are deposited in a continental environment or, more precisely, in an alluvial fan or proximal parts of a braided river system, or in rapid mountain streams during a strong rainfalls. According to their spatial relationship with respect to surrounding Upper Cretaceous granites and rhyolites and Ottnangian sediments; and considering the facies characteristics, we assume that these sediments belong to the Oligocene.

Ključne riječi

Coarse-grained clastics; Continental sediments; Red beds; Oligocene; Mt. Pozeska Gora; Croatia

Hrčak ID:

19937

URI

https://hrcak.srce.hr/19937

Datum izdavanja:

10.6.1993.

Posjeta: 1.286 *