[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
Geochemical characterization of ophiolites in the Alpine-Himalayan Orogenic Belt: Magmatically and tectonically diverse evolution of the Mesozoic Neotethyan …
Ophiolites are important archives of oceanic crust development and preservation in the rock
record, and the Alpine-Himalayan Orogenic Belt (AHOB) is one of the most comprehensive …
record, and the Alpine-Himalayan Orogenic Belt (AHOB) is one of the most comprehensive …
[HTML][HTML] New constraints for the western Paleotethys paleogeography-paleotectonics derived from detrital signatures: Malaguide Carboniferous Culm Cycle (Betic …
Carboniferous sandstone within the Paleo-Mesomediterranean Domain (Malaguide
Subdomain), in southern Spain, represents a key detrital mode within the sedimentary …
Subdomain), in southern Spain, represents a key detrital mode within the sedimentary …
Origin and consequences of western Mediterranean subduction, rollback, and slab segmentation
The western Mediterranean recorded subduction rollback, slab segmentation and
separation. Here we address the questions of what caused Oligocene rollback initiation, and …
separation. Here we address the questions of what caused Oligocene rollback initiation, and …
Tethys–Atlantic interaction along the Iberia–Africa plate boundary: The Betic–Rif orogenic system
Initial SE-dip** slow subduction of the Ligurian–Tethys lithosphere beneath Africa from
Late Cretaceous to middle Oligocene twisting to a later faster E-dip** subduction of the …
Late Cretaceous to middle Oligocene twisting to a later faster E-dip** subduction of the …
The role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism
We summarize the uptake of carbon and sulfur during serpentinization of seafloor
peridotites, and discuss the fate of these volatiles during subduction of serpentinite. We use …
peridotites, and discuss the fate of these volatiles during subduction of serpentinite. We use …
[HTML][HTML] Four billion years of ophiolites reveal secular trends in oceanic crust formation
H Furnes, M De Wit, Y Dilek - Geoscience Frontiers, 2014 - Elsevier
We combine a geological, geochemical and tectonic dataset from 118 ophiolite complexes
of the major global Phanerozoic orogenic belts with similar datasets of ophiolites from 111 …
of the major global Phanerozoic orogenic belts with similar datasets of ophiolites from 111 …
The Tell-Rif orogenic system (Morocco, Algeria, Tunisia) and the structural heritage of the southern Tethys margin
The Tell-Rif (Tell in Algeria and Tunisia; Rif in Morocco) is the orogenic system fringing to
the south the West Mediterranean basins. This system comprises three major tectonic …
the south the West Mediterranean basins. This system comprises three major tectonic …
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain
We use the concentrations and isotope compositions of water, carbon, and sulfur in
serpentinites and their dehydration products to trace the cycling of volatiles during …
serpentinites and their dehydration products to trace the cycling of volatiles during …