A5040026284- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Geological and Geophysical Studies Worldwide
- Geology and Paleoclimatology Research
- Geothermal Energy Systems and Applications
- Geological Formations and Processes Exploration
- CO2 Sequestration and Geologic Interactions
- Geological Modeling and Analysis
- Hydrocarbon exploration and reservoir analysis
- Groundwater and Isotope Geochemistry
- Geological formations and processes
- Geological Studies and Exploration
- 3D Surveying and Cultural Heritage
- Geotourism and Geoheritage Conservation
- Building materials and conservation
- Mineralogy and Gemology Studies
- Geochemistry and Elemental Analysis
- Geomagnetism and Paleomagnetism Studies
- Archaeology and ancient environmental studies
- Clay minerals and soil interactions
- Pleistocene-Era Hominins and Archaeology
- Maritime and Coastal Archaeology
- Facial Trauma and Fracture Management
University of Pisa
2013-2025
Terra
2019
The study of active and fossil hydrothermal systems shows clay minerals to be a fundamental tool for the identification characterization alteration facies. occurrence composition facies could provide useful information on physicochemical conditions activity affecting rock volume. In particular, (i.e., smectite group, chlorite, illite, kaoline pyrophyllite, biotite) are pivotal extrapolating important parameters that strongly affect development water/rock interaction processes such as...
Abstract The benign fuming activity of dormant volcanoes is punctuated by phases escalating degassing that, on some occasions, ultimately prelude to eruption. However, understanding the drivers such unrest complicated complex interplay between magmatic and hydrothermal processes. Some most comprehensively characterised have recently been observed at La Fossa cone Vulcano Island, but whether or not these episodes involve new, volatile-rich ascending magma remains debated. Here, we use...
Research Article| November 01, 2001 Melt inclusion record of immiscibility between silicate, hydrosaline, and carbonate melts: Applications to skarn genesis at Mount Vesuvius Paolo Fulignati; Fulignati 1Dipartimento di Scienze della Terra, Università degli Studi Pisa, via Santa Maria 53, 56126 Italy Search for other works by this author on: GSW Google Scholar Vadim S. Kamenetsky; Kamenetsky 2School Earth Sciences Centre Ore Deposit Research, University Tasmania, GPO Box 252-79, Hobart,...
The thermal and compositional conditions of magma chambers constrain the type complexity their metasomatic aureoles. Fragments these aureoles, disrupted during explosive eruptions Vesuvius, provide quenched snapshots interactions between potassic magmas carbonate country rocks. Near highly crystallized peripheral portions chambers, represented by magmatic xenoliths (fergusites, syenites pyroxenites), skarn aureoles form. Open conduit reservoirs lower plinian subplinian eruption develop...
Abstract: Ischia is a rare case of well-exposed caldera system that has experienced rapid recent resurgence, which can be used to dissect the anatomy an otherwise inaccessible active hydrothermal developed in caldera-forming environment. Integrated analyses melt and fluid inclusions, mineralogy stable isotopic compositions pumices, tuffs syenitic xenoliths volcanic provide strong physico-chemical constraints on shallow magmatic reservoir system. The been exposed by uplift Mt. Epomeo...
In this paper we build a subsurface model that helps in visualizing and understanding the structural framework, geology their interactions with Mt. Amiata geothermal system. Modelling 3D provides possibility to interpolate geometry of structures is an effective way geological features. The modelling approach appears be crucial for further progress reconstruction assessment Amiata. Furthermore, used as basis numerical thermo-fluid-dynamic existing reservoir(s). integration between borehole...