Tracking the isostatic and eustatic signals in an end Ordovician-early Silurian deglacial sedimentary record (Algeria - Libya border)

Author:

Girard Flavia1,Deschamps Rémy2,Ghienne Jean-François3,Roussé Stéphane4,Rubino Jean-Loup5

Affiliation:

1. Géosciences Montpellier; UMR5243; Université de Montpellier; CC.60, place E. Bataillon 34095 Montpellier Cedex France

2. IFP Energies Nouvelles; 1 and 4, avenue de Bois-Préau 92852 Rueil Malmaison France

3. IPGS, UMR7517, CNRS; Université de Strasbourg; 1 rue Blessig 67084 Strasbourg France

4. BEICIP-FRANLAB; 232 Av. Napoléon Bonaparte 92500 Rueil Malmaison France

5. TOTAL; Avenue Larribau 64018 Pau Cedex France

Funder

Agence Nationale de la Recherche

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference111 articles.

1. Shallow marine trace fossils from upper Devonian sediments of the Kuh-E Zard, Zefreh area, Central Iran;Abbassi;Iran. J. Sci. Technol. Trans. A Sci.,2007

2. Sand waves: a model of origin and internal structure;Allen;Sed. Geol.,1980

3. Paraglacial geomorphology;Ballantyne;Quatern. Sci. Rev.,2002

4. Contrasting glacial sedimentation processes and sea-level changes in two adjacent basins on the Pacific margin of Canada;Barrie;Geol. Soc. Lond. Spec. Publ.,2002

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