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Abstract

Nummulitic limestones in the Gulf of Gabes and onshore Central Tunisia i.e. the Early Eocene (Ypresian) El Garia Formation and the Mid-Eocene Reineche Member are generally interpreted as hydrodynamic storm-derived nummulite accumulations. Such models try to explain the characteristic irregular bedding and scattering of nummulites by the occurrence of chaotic turbulent current patterns during storm events.

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/content/papers/10.3997/2214-4609.201406067
2000-10-01
2021-12-09
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406067
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