The central-western Mediterranean area is a key region for understanding the complex
interaction between igneous activity and tectonics. In this review, the specific geochemical …

The widely debated late Oligocene-middle Miocene Numidian Fm (NF) consists of
supermature quartzose sediments deposited in the Maghrebian Flysch Basin (MFB) …

We present a geodynamic reconstruction of the Central–Western Mediterranean and
neighboring areas during the last 50Myr, including magmatological and tectonic …

Abstract The Bou Jaber Ba-F-Pb-Zn deposit is located at the edge of the Bou Jaber Triassic
salt diapir in the Tunisia Salt Diapir Province. The ores are unconformity and fault-controlled …

A comparison of the stratigraphic record between two different branches of the Tethys is
attempted for the first time. This study concerns the main Oligocene-Miocene tectono …

A synthetic study has been made to identify main tectono-sedimentary and geodynamic
events in central-western Tethys. For this, an interdisciplinary analysis has been performed …

Two orthogonal extensional systems produced the extensional collapse of the Tell and Atlas
thrust belts in northern Tunisia during the Late Miocene to Pliocene in a context of NW‐SE …

A review of the paleogeographic and tectonic reconstruction of the onshore and offshore
Tunisian margin during the Cenozoic is discussed. Five unconformities (A to E) and …

The provenance of the Numidian Flysch in the western Mediterranean remains a
controversial subject which hinders understanding of this regionally widespread …

We determine the deep structure of the eastern Algerian basin and its southern margin in the
Annaba region (easternmost Algeria), to better constrain the plate kinematic reconstruction …