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Manuel Francisco Pereira

Researcher at University of Évora

Publications -  88
Citations -  2066

Manuel Francisco Pereira is an academic researcher from University of Évora. The author has contributed to research in topics: Zircon & Massif. The author has an hindex of 24, co-authored 84 publications receiving 1710 citations. Previous affiliations of Manuel Francisco Pereira include University of Lisbon & Technical University of Lisbon.

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Influence of the Aerodynamic Forces on the Pantograph-Catenary System for High Speed Trains

TL;DR: In this paper, a detailed multibody model of the catenary and the pantograph is presented for the identification of the dynamic behaviour of the pantographs and of the interaction phenomena in the catenaries of high-speed trains due to the action of aerodynamics forces.
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North-Gondwana assembly, break-up and paleogeography: U–Pb isotope evidence from detrital and igneous zircons of Ediacaran and Cambrian rocks of SW Iberia

TL;DR: The Estremoz Anticline in the Ossa-Morena Zone (SW Iberia) includes upper Ediacaran detrital rocks unconformably overlain by lower Cambrian carbonate and carbonate rocks as discussed by the authors.
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Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone (Evora-Aracena metamorphic belt, SW Iberian Massif): Sm-Nd isotopes and SHRIMP zircon U-Th-Pb geochronology

TL;DR: In this paper, Detrital zircon from the Serie Negra sediments of the Evora-Aracena metamorphic belt, Ossa-Morena Zone, SW Iberian Massif, preserve a record of the erosion of an Avalonian-Cadomian magmatic arc and subsequent related turbiditic sedimentation.
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The provenance of Late Ediacaran and Early Ordovician siliciclastic rocks in the Southwest Central Iberian Zone: constraints from detrital zircon data on northern Gondwana margin evolution during the late Neoproterozoic

TL;DR: U-Pb geochronology of detrital zircon from Late Ediacaran (Beiras Group greywackes) and Early Ordovician (Sarnelhas arkosic quartzites and Armorican quartzites of Penacova) sedimentary rocks of the southwest Central Iberian Zone (SW CIZ) constrain the evolution of northern Gondwana activepassive margin transition as discussed by the authors.
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Rift-related volcanism predating the birth of the Rheic Ocean (Ossa-Morena zone, SW Iberia)

TL;DR: In this paper, the early and main events in the Ossa-Morena zone of SW Iberia have been interpreted to have culminated in the opening of the Rheic Ocean during the Early Ordovician.