A5066702994- Geological and Geochemical Analysis
- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- Archaeological and Geological Studies
- Geology and Paleoclimatology Research
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Elemental Analysis
- High-pressure geophysics and materials
- Geological formations and processes
- Hydrocarbon exploration and reservoir analysis
- Cerebrovascular and Carotid Artery Diseases
- Landslides and related hazards
- Acute Ischemic Stroke Management
- Meat and Animal Product Quality
- Groundwater and Isotope Geochemistry
- Intestinal and Peritoneal Adhesions
- Science and Science Education
- Evolution and Paleontology Studies
- Karst Systems and Hydrogeology
- Venous Thromboembolism Diagnosis and Management
- Italian Fascism and Post-war Society
- Pleistocene-Era Hominins and Archaeology
- European history and politics
National Laboratory of Energy and Geology
2013-2024
Biogipuzkoa Health Research Institute
2022
Departamento de Ciência e Tecnologia
2013
Terra
2013
National Institute of Engineering, Technology and Innovation
2008-2010
Abstract The recently discovered massive and stockwork sulphide mineralization of Semblana-Rosa Magra Monte Branco, situated ESE the Neves–Corvo volcanogenic (VMS) deposit in Iberian Pyrite Belt (IPB) is presented. Geological setting tectonic model discussed based on proxies such as palynostratigraphy U–Pb zircon geochronology. found within IPB Volcano-Sedimentary Complex (VSC) Lower sequence, which includes felsic volcanic rocks (rhyolites) with ages zircons 359.6 ± 1.6 Ma, black shales...
This work assessed the age distribution of Cadomian/Pan-African orogenic events (550-590 and 605-790Ma, respectively) in several zones Iberian Massif by means detrital inherited zircon analysis compilation.
Abstract Research is described to evaluate the influence of volcanic activity on studies shell-concentration taphonomy and biodiversity patterns in strata that commonly display poor densities skeletal debris. Two episodes are recorded Lower Ordovician Iberian Chains: (i) a succession Tremadocian-earliest “Arenig”, eruptive felsic products, expelled explosively characterized by onset rhyolitic dacitic tuffs embedded Borrachón Santed formations; (ii) an effusive basaltic episode, represented...
Despite the so-called exotic nature of South Portuguese Zone relatively to other major domains Iberian Massif peri-Gondwanan affinity, Devonian detrital rocks oldest strata in Pyrite Belt have a remarkable resemblance with Ossa-Morena Zone’s Neoproterozoic-Cambrian and West Meguma’s Cambrian-Ordovician rocks, presenting “West African signature”.
Abstract This work investigates the relationships between partial melting, melt extraction, pluton growth and silicic volcanism in garnet-bearing felsic volcanic rocks that were extruded Iberian Pyrite Belt, at ca . 345 Ma. The garnets are of peritectic origin, displaying textural chemical features disequilibrium crystallization during melting reactions involving biotite high temperatures (up to 870 °C) middle-lower crust. Major element composition suggests compositional equilibrium with...