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P. Farias

Researcher at University of Oviedo

Publications -  34
Citations -  1157

P. Farias is an academic researcher from University of Oviedo. The author has contributed to research in topics: Paleozoic & Permian. The author has an hindex of 17, co-authored 32 publications receiving 1012 citations.

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Diachronous Variscan tectonothermal activity in the NW Iberian Massif: Evidence from 40Ar/39Ar dating of regional fabrics

TL;DR: In this article, multigrain concentrates of hornblende and muscovite together with whole-rock slate/phyllite samples have been dated using 40Ar/39Ar incremental-release methods along a systematic traverse across the various lithotectonic structural elements which comprise northwestern sectors of the Variscan Iberian Massif.
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The last deglaciation in the Picos de Europa National Park (Cantabrian Mountains, northern Spain)

TL;DR: In this paper, a sedimentological and geochemical study of the Lago Enol sequence (Cantabrian Mountains, northern Spain), together with detailed geomorphological mapping, provides a first record of glacier evolution and climate change over the last 40 ka in the Picos de Europa National Park.
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A review of glacial geomorphology and chronology in northern Spain: Timing and regional variability during the last glacial cycle

TL;DR: In this paper, the authors synthesize the research in glacial geomorphology and geochronology in northern Spain, with special attention to the evidence of local glacier maximum extent earlier than the global LGM of MIS 2 (18-21-ka BP).
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Emplacement of the Cuera and Picos de Europa imbricate system at the core of the Iberian-Armorican arc (Cantabrian zone, north Spain): New precisions concerning the timing of arc closure

TL;DR: In this paper, it was shown that the thrust sheets were emplaced roughly perpendicular to previous tectonic units of the Cantabrian Variscan foreland fold-and-thrust belt, most probably during the oroclinal bending of the SW European variscan belt that formed the Iberian-Armorican arc.
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The Basement of the Andean Frontal Cordillera in the Cordón del Plata (Mendoza, Argentina): Geodynamic Evolution

TL;DR: The Andean Paleozoic basement of the Cordon del Plata (Argentina) consists of two sets of rocks showing different stratigraphy, structure and metamorphism.