Tethys–Atlantic interaction along the Iberia–Africa plate boundary: The Betic–Rif orogenic system
J Vergés, M Fernàndez - Tectonophysics, 2012 - Elsevier
Initial SE-dipping slow subduction of the Ligurian–Tethys lithosphere beneath Africa from
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …
Provenance and source-to-sink of lower-middle Jurassic sediments from Hinterland mounts to NW-Gondwana hyper-extended passive margin (Prerif sub-domain …
H Kairouani, MN Zaghloul, A Abbassi… - Marine and Petroleum …, 2023 - Elsevier
The present work deals with the provenance of lower-middle Jurassic successions
belonging to the External Prerif Foreland basin, which remains till now misunderstood and …
belonging to the External Prerif Foreland basin, which remains till now misunderstood and …
Tectonic and stratigraphic evolution of the Western Alboran Sea Basin in the last 25 Myrs
Abstract The Western Alboran Basin (WAB) formation has always been the subject of debate
and considered either as a back-arc or a forearc basin. Stratigraphic analyses of high …
and considered either as a back-arc or a forearc basin. Stratigraphic analyses of high …
Wealth of P–T–t information in medium-high grade metapelites: Example from the Jubrique Unit of the Betic Cordillera, S Spain
HJ Massonne - Lithos, 2014 - Elsevier
It is demonstrated here that medium-high grade metapsammopelites contain a wealth of
information to derive a well-constrained P–T–t path relevant for the understanding of the …
information to derive a well-constrained P–T–t path relevant for the understanding of the …
Extreme extension across Seram and Ambon, eastern Indonesia: evidence for Banda slab rollback
The island of Seram, which lies in the northern part of the 180°-curved Banda Arc, has
previously been interpreted as a fold-and-thrust belt formed during arc-continent collision …
previously been interpreted as a fold-and-thrust belt formed during arc-continent collision …
Pre-Alpine prograde evolution of the Upper Alpujarride (Betic-Rif belt) reveals a Paleotethys-related collision
A Sánchez-Navas, A Martín-Algarra… - International Geology …, 2024 - Taylor & Francis
Medium and high grade kyanite-bearing graphitic metapelites of the basement of the Torrox
Unit (Upper Alpujarride, Western Mediterranean) show kyanite-andalusite-kyanite …
Unit (Upper Alpujarride, Western Mediterranean) show kyanite-andalusite-kyanite …
Polyphase tectonic evolution of fore‐arc basin related to STEP fault as revealed by seismic reflection data from the Alboran Sea (W‐Mediterranean)
Since the Miocene, the thinned continental crust below the Alboran Sea and its overlying
sedimentary cover have been undergoing deformation caused by both convergence of …
sedimentary cover have been undergoing deformation caused by both convergence of …
The Beni Bousera peridotite (Rif Belt, Morocco): an oblique-slip low-angle shear zone thinning the subcontinental mantle lithosphere
Detailed structural and petrological mapping in the Beni Bousera peridotite (Rif Belt,
northern Morocco) shows that this orogenic peridotite massif is composed of four tectono …
northern Morocco) shows that this orogenic peridotite massif is composed of four tectono …
Deformation and exhumation of the Ronda peridotite (Spain)
The Ronda peridotite supplies one of the best objects to document subcontinental mantle
deformation, but its internal deformation and exhumation mechanisms remain controversial …
deformation, but its internal deformation and exhumation mechanisms remain controversial …
Oligo‐Miocene thinning of the Beni Bousera peridotites and their Variscan crustal host rocks, Internal Rif, Morocco
Abstract Deciphering Variscan versus Alpine history in the Internal Rif system is a key to
constrain the tectonic evolution of the Alboran domain and hence the geodynamics of the …
constrain the tectonic evolution of the Alboran domain and hence the geodynamics of the …