Diagenetic process as tool to diagnose paleo-environment conditions, bathymetry and oxygenation during Late Paleocene-Early Eocene in the Gafsa Basin

Author:

Messadi Abdel Majid,Mardassi Besma,Ouali Jamel Abdennaceur,Touir Jamel

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference90 articles.

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2. Adatte T, Lu G (1995) Clay mineral correlation across the Paleocene-Eocene boundary: evidence of global turnover from western to eastern Tethys. In: Geological Society of America 1995, Annual Meeting, New Orleans, USA. Abstract p. 405

3. Ahmed AH, Tlili A, Zalat A, Jeddoui Y (2014) Fossil diatoms from endogangue of the Ypresian phosphatic pellets of the Gafsa-Metlaoui basin: implication on the origin of biogenic silica and depositional environment. J Geosci Arab. https://doi.org/10.1007/s12517-013-1253-2

4. Ali MBH, Kadri A, Zagrarni MF, Gaied M E (2002) Les unités lithostratigraphiques de l’Eocène en Tunisie: Evolution latérale et actualisation de la nomenclature-. Notes du Service Géologique de Tunisie, 69:53–73

5. Assereto R, Folk RL (1980) Diagenetic fabrics of aragonite, calcite, and dolomite in an ancient peritidal-spelean environment: Triassic Calcare Rosso, Lombardia, Italy. J Sediment Res 50(2):371–394

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