Geologia Croatica, Vol. 45 No. 1, 1992.
Izvorni znanstveni članak
https://doi.org/10.4154/GC.1992.06
The Bottom Current Sediments (Contourites) in the Upper Cretaceus Deep-Water Deposits in the Northeeastern Part of Žumberak (Croatia)
Ervin Mrinjek
; Department of Geology and Paleontology, Faculty of Sciences, University of Zagreb
Sažetak
The Upper Cretaceous deep marine deposits in NE parts of Žumberak contain sediments deposited by bottom currents - muddy, sandy and sandy-gravelly contourites. The complete (negative-positive) sequences and incomplete (negative-positive) sequences have been observed.Apart from the sediments that have been deposited by bottom currents,several turbidite layers reworked by bottom currents occur.
Ključne riječi
contourites; contour sequences; bottom currents; turbidites; hemipelagites; deep-water deposits, Upper Cretaceous; Žumberak; Dinarides
Hrčak ID:
183544
URI
Datum izdavanja:
20.8.1992.
Posjeta: 574 *