Abstract The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the
subduction of the Alpine Tethys and the later collision of drifted continental blocks against …

Over the last years, the global application of machine learning (ML) models in groundwater
quality studies has proved to be a robust alternative tool to produce highly accurate results …

Abstract The Maghreb region (from Tunisia to Gibraltar) is a key area in the western
Mediterranean to study the active tectonics and stress pattern across the Africa‐Eurasia …

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 …

Tunisia, located in the Northern African margin, was subjected to Late Permian-Early
Cretaceous N–S extension subsequent to Pangea breakup and leading to the Tethyan …

Cenozoic extension in the Western Mediterranean has been related to the dynamics of back‐
arc domains. Although, in most of its orogenic belts extension propagated into the fore‐arc …

Abstract Active tectonics in North Africa are fundamentally driven by NW-SE directed slow
convergence between the Nubia and Eurasia plates, leading to a region of thrust and strike …

Mineralization processes in the Tell-Atlas of North Africa coincided with magmatism,
extension, and lithospheric rejuvenation during the middle to late Miocene. This review …

Active shortening structures in Northern Tunisia have developed by tectonic inversion since
the Pliocene, after Late Miocene extensional collapse of the whole region. Restored Plio …

This paper resolves the structural complexity of Cenozoic sedimentary basins in
northeastern Tunisia. These basins trend NE-SW to∼ EW, and are bordered by old fracture …