A5091015812- Geological and Geochemical Analysis
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- Seismology and Earthquake Studies
- Earthquake Detection and Analysis
- Geological and Geophysical Studies Worldwide
- High-pressure geophysics and materials
- Paleontology and Stratigraphy of Fossils
- Geological Formations and Processes Exploration
- Hydrocarbon exploration and reservoir analysis
- Seismic Waves and Analysis
- Ancient Mediterranean Archaeology and History
- Time Series Analysis and Forecasting
- Reservoir Engineering and Simulation Methods
- Geological and Tectonic Studies in Latin America
- Maritime and Coastal Archaeology
- Archaeology and ancient environmental studies
Istituto Nazionale di Geofisica e Vulcanologia
2023-2024
INGV Sezione di Milano
2023
University of Parma
2021-2023
Seismic signals coupling to physical (e.g., temperature, pH, Eh, electrical conductivity, flow rate) and geochemical changes in ground spring waters as well variations soil flux regimes CO2, CH4, radon) represent a valuable tool better understand the interaction between tectonics crustal fluids dynamics Italiano et al., 2001, 2004; Wang Manga, 2021; Chiodini 2020; Gori Barberio, 2022 references therein). Pre-, co- post-seismic modifications are markers of local tectonic stress acting crust...
The present work would like to illustrate a new concept of multiparametric stations characterize the crustal fluids-tectonic interaction in specific geological contexts. dynamics fluids relation tectonics is complex and sometimes intricate issue. Several factors act mutually influence themselves, so that each tectonic context they follow behavior, comprehensive cause-effect rule hard find. Changes water chemistry levels soil flux regimes (e.g., CO 2 , CH 4 radon) are just few examples well...
Abstract. In this paper, the new dynamic geophysical and geochemical MUltiparametric DAtabase (MUDA) is presented. MUDA a infrastructure of National Institute Geophysics Volcanology (INGV), published on-line in December 2023, with aim archiving disseminating multiparametric data collected by multidisciplinary monitoring networks. MySQL relational database web interface developed php, aimed at investigating quasi real time possible correlations between seismic phenomena variations endogenous...
The New Caledonia Ophiolite is cross-cut by coarse- to medium-grained pyroxenite and hornblende gabbro/diorite dykes intruded between 55.5 50 Ma (U–Pb zircon 40 Ar/ 39 Ar hornblende), whereas the finer grained dolerites of tholeiitic affinity are younger (50–47 Ma). production gabbros/diorites was modelled moderate degrees (20–40%) partial melting high-temperature amphibolites metamorphic sole. end-member compositions (hornblendites anorthosites) resulted from solid-state phase segregation...
MUDA (geophysical and geochemical MUltiparametric DAtabase) is a new infrastructure of the National Institute Geophysics Volcanology (INGV, www.ingv.it) serving geophysical multiparametric data, designed developped in framework Dynamic Planet -Working Earth project (https://progetti.ingv.it/it/pian-din).MUDA dynamic relational database based on MySQL (https://www.mysql.com) with web interface realised php (https://www.php.net) using responsive design technique. The multi-parametric data are...
Abstract. In this paper, the new dynamic geophysical and geochemical MUltiparametric DAtabase (MUDA) is presented. MUDA a infrastructure of National Institute Geophysics Volcanology (INGV), published online in December 2023, with aim archiving disseminating multiparametric data collected by multidisciplinary monitoring networks. MySQL relational database web interface developed PHP, aimed at investigating possible correlations between seismic phenomena variations endogenous environmental...
<p>Pyroxenites constitute the major form of heterogeneity in upper mantle. Their occurrence supra-subduction zone settings is mostly testified by veins and layers refractory ophiolitic peridotites, where they represent a crucial witness melt migration forearc/subarc environment [1,2]. The New Caledonia ophiolite hosts one largest forearc mantle section worldwide, providing unique perspective into processes. sequence dominated ultra-depleted harzburgites [3], locally overlain...
<p>The New Caledonia ophiolite hosts one of most complete sections a nascent arc, representing an excellent natural laboratory for investigating the origin and evolution subduction systems. The sequence, originated during onset Eocene [1, 2], is composed ultra-depleted forearc harzburgites [3] overlain by dunite-dominated transition zone (500m thick), in turn overtopped mafic-ultramafic cumulate lenses. ultramafic rocks (mainly dunites wehrlites) likely resulted from...