The Atlas Mountains are classically regarded as a failed Mesozoic rift arm subject to Alpine
inversion, folding and thrusting. Here, we present new integrated structural and …

Abstract The central High Atlas (Morocco) constitutes a diapiric province that hosts a
complex array of elongated diapirs and minibasins that formed during the Lower Jurassic rift …

This article presents an overview of regional extensional deformation across the north-facing
southern Tethyan continental passive margin of Tunisia during the Aptian and Albian syn-rift …

Based on new structural, sedimentary, stratigraphic and seismic reflection data from
Cretaceous sequences of the Zemlet el Beidha anticline of the northern Chotts range (South …

Surface and subsurface data together with balanced cross-sections are used to emphasize
the structural style and regional-scale deformation of the Southern Atlas Front in Tunisia and …

The structure of the southern Atlas fold-and-thrust belt of Tunisia was investigated using new
geologic mapping, seismic reflection data together with the construction of a balanced cross …

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 …

Detailed geologic mapping, structural analysis, field cross-sections, new dating based on
planktonic foraminifera, in addition to gravity signature of Lorbeus diapir, are used to …

We present a regional-residual separation procedure for potential field data (gravity or
magnetic) based on the integration of least-squares polynomial, power density spectrum …

Detailed geological mapping, dating, and gravimetric and seismic data are used to interpret
the Lansarine–Baouala salt structure (North Tunisia) as a salt canopy emplaced during the …