A5084039159- Geological and Geophysical Studies Worldwide
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Archaeological and Geological Studies
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Geologic Mapping
- Archaeological and Historical Studies
- Geological and Tectonic Studies in Latin America
- Power Line Communications and Noise
- Millimeter-Wave Propagation and Modeling
- Geological formations and processes
- Advanced MIMO Systems Optimization
- Cellular Automata and Applications
- Karst Systems and Hydrogeology
- Geology and Paleoclimatology Research
- Advanced Wireless Communication Techniques
- Wireless Communication Networks Research
- Geological Studies and Exploration
- Theoretical and Computational Physics
- Quantum chaos and dynamical systems
- Geotechnical and Geomechanical Engineering
- Optical Network Technologies
- Advanced Fiber Laser Technologies
- Advanced Photonic Communication Systems
- Slime Mold and Myxomycetes Research
University of Trás-os-Montes and Alto Douro
2002-2025
Universidade Federal do Rio de Janeiro
2024
Hospitais da Universidade de Coimbra
2023
University of Lisbon
2008-2022
Centro Interuniversitário de História das Ciências e da Tecnologia
2016-2022
Museu Nacional de História Natural e da Ciência
2016-2022
Instituto Dom Luiz
2019-2021
Universidade Estadual de Campinas (UNICAMP)
2006-2016
Polytechnic Institute of Bragança
2015
National Archaeology Museum
2009
The early evolution of SW Europe Variscides started by opening the Rheic ocean at ∼500 Ma, splitting Avalonia from Armorica/Iberia. Subduction on SE side generated Paleotethys back‐arc basin (430–390 Armorica Iberia), with development Porto‐Tomar‐Ferreira do Alentejo (PTFA) dextral transform defining boundary between continental and Finisterra microplate to W. Obduction was followed Armorica/Iberia collision emplacement NW Iberian Allochthonous Units 390–370 whereas toward west PTFA, there...
Research Article| August 01, 2013 Are subduction zones invading the Atlantic? Evidence from southwest Iberia margin João C. Duarte; Duarte 1School of Geosciences, Monash University, Melbourne, Victoria 3800, Australia Search for other works by this author on: GSW Google Scholar Filipe M. Rosas; Rosas 2Departamento de Geologia, Faculdade Ciências da Universidade Lisboa, 1749-016 Lisbon, Portugal3Instituto Dom Luiz, Portugal Pedro Terrinha; Terrinha Portugal4Instituto Português do Mar e...
The Portuguese mainland territory is located close to the Azores‐Gibraltar plate boundary, in a tectonic setting responsible for significant neotectonic and seismic activities. However, few data concerning present regional lithospheric stress field were available, as testified by recently published maps of indicators Europe Mediterranean regions. One authors already presented synthesis on this subject [ Cabral , 1993], where geological geophysical considered. In paper we introduce new...
On November 1, 1755, the city of Lisbon was completely devastated by combined effect a tremendous earthquake, tsunami waves, and fire. The 1755 earthquake most destructive cataclysm recorded in western Europe since Roman Republic, with an estimated magnitude M w ∼8.5 [ Martins Mendes Victor , 1990] t = 8.5. felt as far away Great Britain Finland. hit many coastal cities along southwest Iberia North Africa, causing heavy destruction Tanger Casablanca.
J. Brilha, C. Andrade, A. Azerêdo, F.J.A.S. Barriga, M. Cachão, H. Couto, P.P. Cunha, J.A. Crispim, P. Dantas, L.V. Duarte, M.C. Freitas, H.M. Granja, M.H. Henriques, L. Lopes, Madeira, J.M.X. Matos, F. Noronha, Pais, Piçarra, M.M. Ramalho, J.M.R.S. Relvas, Ribeiro, Santos, V.F. Terrinha. Episodes 2005;28:177-86. https://doi.org/10.18814/epiiugs/2005/v28i3/004
The catalytic esterification of levulinic acid (LA) to methyl levulinate (ML) was investigated using copper molybdate (Cu3(MoO4)2(OH)2) as a heterogeneous catalyst. catalyst, synthesized via chemical precipitation, exhibited monoclinic structure with self-assembled nanoplates forming spherical mesostructures. Structural characterization confirmed its high crystallinity, while textural analysis revealed BET surface area 70.55 m2 g−1 pore sizes in the nanometric range (1–6 nm). performance...
Evidence for three short‐lived compressive episodes of late Carixian, Callovian–early Oxfordian, and Tithonian‐Berriasian ages that lasted <5 m.yr. occurred during the process rifting Algarve Basin is presented. These tectonic‐inversion are described at outcrop cartographic scales have been dated with accuracy provided by ammonoid scale. An uplift event Toarcian–Aalenian age undetermined tectonic origin also described. We show these four coincide in time important ecological events, such as...