The Algerian margin formed through back-arc opening of the Algerian basin (Mediterranean
Sea) resulting from the roll-back of the Tethyan slab. Recent geophysical data acquired …

In the Chelif basin, the geochemical characterization reveals that the Upper Cretaceous and
Messinian shales have a high generation potential. The former exhibits fair to good TOC …

Abstract The Anambra Basin in the west of the lower Benue Trough is one of Nigeria's most
petroliferous provinces. The subsurface structure has been extensively studied using …

Field gravimetric and stratigraphic surveys were conducted with the aim to constraint the
mechanisms responsible for the initiation of the Stenian-Tonian Paranoá basin, central …

The existence of several magnitude scales in the compiled earthquake catalogs of a specific
region has made the development of regional relations connecting magnitude scales a …

Abstract The Chelif Basin (North Algeria) is one of the most seismically active zones of the
western Mediterranean Sea. It constitutes a key area to study neotectonic structures and …

The Chlef region constitutes a key area to study neotectonics structures and their
geodynamical context. Aeromagnetic data analyzed using different processing methods …

The northern Algeria forms the southern edge of the Western Mediterranean Sea that formed
within the zone of convergence between the African and Eurasian plates. It represents a key …

We determine the structural architecture of the hydrothermal system of Hammam Bouhadjar
area (Northwest of Algeria) by the use of geophysical data. New gravity and electrical …

The crustal structure beneath the northeastern continental part of Algeria is still largely
unknown. Here we use potential field data processing, modeling and interpretation in order …