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Lj. Babić J. Zupanič M. Crnjaković - 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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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)

Lj. Babić
J. Zupanič
M. Crnjaković

Puni tekst: engleski, pdf (12 MB)str. 107-123preuzimanja: 351*citiraj

Sažetak
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.

Ključne riječi
Marine clasticsCross-bedded sandstonesCross-laminated sandstonesGravity flow depositsEoceneIsland of PagOuter Dinarides

Hrčak ID: 19935

URI
https://hrcak.srce.hr/19935

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