An Association of Marine Tractive and Gravity Flow Sandy Deposits in the Eocene of the NW Part of the Island of Pag (Outer Dinarides, Croatia)

The Eocene clastics of the NW part of the island of Pag overlie carbonate platform deposits and are dominantly sandy. Besides minor components, they include cross-laminated and cross-bedded sandstones produced by marine tractive flows, mostly directed toward E, and ESE, and dominantly massive sandst...

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Published in:Geologia Croatica 2010-12, Vol.46 (1), p.107-123
Main Authors: Ljubomir Babić, Jožica Zupanič, Marta Crnjaković
Format: Article
Language:English
Subjects:
Cross-bedded sandstones
Cross-laminated sandstones
Eocene
Gravity flow deposits
Island of Pag
Marine clastics
Outer Dinarides
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Jožica Zupanič
Marta Crnjaković
description The Eocene clastics of the NW part of the island of Pag overlie carbonate platform deposits and are dominantly sandy. Besides minor components, they include cross-laminated and cross-bedded sandstones produced by marine tractive flows, mostly directed toward E, and ESE, and dominantly massive sandstones probably deposited by gravity flows. The area was situated close to sand-rich sources and river mouth(s). Possible settings include a delta-related shallow-marine area, and a sea strait. Structural deformation intervened very early in the history of a complex outer dinaric foreland realm and governed its subsequent evolution, in contrast to a simple foreland trough envisaged before.
doi_str_mv 10.4154/GC.1993.09
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ispartof Geologia Croatica, 2010-12, Vol.46 (1), p.107-123
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language eng
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subjects Cross-bedded sandstones
Cross-laminated sandstones
Eocene
Gravity flow deposits
Island of Pag
Marine clastics
Outer Dinarides
title An Association of Marine Tractive and Gravity Flow Sandy Deposits in the Eocene of the NW Part of the Island of Pag (Outer Dinarides, Croatia)
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