The Bottom Current Sediments (Contourites) in the Upper Cretaceus Deep-Water Deposits in the Northeeastern Part of Žumberak (Croatia)

Article Sidebar

PDF
Published: Dec 2, 2010
DOI: https://doi.org/10.4154/GC.1992.06
Keywords:
contourites, contour sequences, bottom currents, turbidites, hemipelagites, deep-water deposits, Upper Cretaceous, Žumberak, Dinarides.

Main Article Content

Ervin Mrinjek
Department of Geology and Palaeontology, Faculty of Science

Abstract

The Upper Cretaceous deep marine deposits in NE parts of Žumberakcontain sediments deposited by bottom currents - muddy, sandy andsandy-gravelly contourites. The complete (negative-positive) sequencesand 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.

Downloads

Download data is not yet available.

Article Details

Issue
Vol 45 (1992)
Section
Original Scientific Papers

Authors have copyright and publishing rights on all published manuscripts.