Data for: Storm-dominated shallow-marine carbonates of the lower Eocene succession of the northwestern Tunisian domain
Published: 30 August 2019| Version 1 | DOI: 10.17632/s75y542t92.1
Contributor:
fehmy belghouthiDescription
The lower Eocene carbonate succession in the Mateur-Beja area, NW of Tunisia, is interpreted as deposited by storm.
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Categories
Sedimentology, Ichnofossils