Small-scale sedimentary structures and their implications in recognizing large-scale ancient tidal bedforms. Example from Dur At Talah outcrop, Late Eocene, Sirt Basin, Libya

Author:

Abouessa Ashour,Duringer Philippe,Schuster Mathieu,Pelletier Jonathan,Rubino Jean-Loup

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference84 articles.

1. Tectonic and subsidence evolution of the Sirt Basin, Libya;Abadi;AAPG Bull.,2008

2. New insight into the sedimentology and stratigraphy of the Dur At Talah tidal–fluvial transition sequence (Eocene–Oligocene, Sirt Basin, Libya);Abouessa;J. Afr. Earth Sci.,2012

3. Ahlbrandt, T.S., 2002. The Sirte Basin Provinces of Libya, Sirte-Zelten total petroleum system. US Geological Survey Bulletin 2202-F, pp. 1–29.

4. Lower cretaceous tides revealed by cross-bedding with mud drapes;Allen;Nature,1981

5. Mud drapes in sand-wave deposits: a physical model with application to the Folkestone beds (Early Cretaceous, Southeast England);Allen;Philos. Trans. Roy. Soc. Lond., Ser. A, Math. Phys. Sci.,1982

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