Results 101 to 110 of about 8,012 (220)
Bimodal magmatism as a consequence of the post-collisional readjustment of the thickened Variscan continental lithosphere (Aiguilles Rouges-Mont Blanc Massifs, Western Alps) [PDF]
: High Precision U-Pb zircon and monazite dating in the Aiguilles Rouges-Mont Blanc area allowed discrimination of three short-lived bimodal magmatic pulses: the early 332 Ma Mg-K Pormenaz monzonite and associated 331 Ma peraluminous Montées Pélissier ...
Bussy, François +2 more
core
40Ar/39Ar laserprobe dating of mylonitic fabrics in a polyorogenic terrane of NW Iberia [PDF]
The tectonothermal evolution of a polyorogenic terrane in the Variscan belt of NW Spain has been constrained by 40Ar/39Ar laserprobe incremental heating experiments on mylonitic fabrics developed in major structures.
Abati Gómez, Jacobo +6 more
core
Seismic anisotropy beneath southern Iberia from SKS splitting [PDF]
International audienceSeismic anisotropy of the south Iberian upper mantle is investigated using shear-wave splitting of SKS phases. We analyzed teleseismic events recorded by sixteen permanent broadband stations installed on the southern Iberian ...
Barruol, Guilhem +3 more
core +2 more sources
The Long-Lasting Exhumation History of the Ötztal-Stubai Complex (Eastern European Alps): New Constraints from Zircon (U–Th)/He Age-Elevation Profiles and Thermokinematic Modeling [PDF]
The Eastern European Alps formed during two orogenic cycles, which took place in the Cretaceous and Cenozoic, respectively. In the Ötztal-Stubai Complex—a thrust sheet of Variscan basement and Permo-Mesozoic cover rocks—the record of the first (Eoalpine)
Kyra Hölzer +3 more
doaj +1 more source
The El Crispinejo granite forms part of a small, but distinctive late intrusive suite of cordierite-bearing peraluminous granites in the South Portuguese Zone (SPZ). This granite has the best outcrop relationships of the suite.
A. DÍEZ MONTES +3 more
doaj
The mineralization processes in the Peloritani Belt (Southern Sector of the Calabria- Peloritani Arc) prevalently developed during the Variscan orogenesis producing Pb, Zn, Fe, As, Sb, Cu, Ag, W, etc. polymetalliferous ore-bearing horizons.
Pisacane, G +4 more
doaj +1 more source
Deciphering orogeny: a metamorphic perspective. Examples from European Alpine and Variscan belts
AbstractIn this paper we review and discuss, in a synthetic historical way, the main results obtained on Alpine metamorphism in the western Alps. First, we describe the finite metamorphic architecture of the western Alps and discuss its relationships with subduction and collision processes.
openaire +1 more source
The architecture of the crust in the French Massif Central (FMC) is described as a nappe stack composed, from top to bottom, of the Upper Gneiss Unit (UGU), the Lower Gneiss Unit (LGU), and the Para-Autochthonous Unit (PAU), which are intruded by ...
Passos do Carmo Caliméria +6 more
doaj +1 more source
Lithospheric structure and tectonic memory of the European Variscan belt
The Variscan belt of Europe formed during the late Paleozoic through the convergence of Laurussia and Gondwana, subduction of intervening oceans, and the accretion of peri-Gondwanan terranes during Pangaea assembly. This study integrates geological, geophysical and crust–mantle structural data to investigate the orogen's construction, destruction and ...
Stanislaw Mazur +4 more
openaire +1 more source
This paper presents and discusses new geochronological and petrological data on a suite of calc-alkaline plutons composed predominantly of diorites and tonalites from the West Massif Central.
Berger Julien +8 more
doaj +1 more source

