A5078177497- Groundwater and Isotope Geochemistry
- Methane Hydrates and Related Phenomena
- Geochemistry and Geologic Mapping
- Atmospheric and Environmental Gas Dynamics
- Hydrocarbon exploration and reservoir analysis
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- CO2 Sequestration and Geologic Interactions
- Radioactivity and Radon Measurements
- Marine and environmental studies
- Heavy metals in environment
- Geochemistry and Elemental Analysis
- Atmospheric chemistry and aerosols
- Groundwater flow and contamination studies
- Lichen and fungal ecology
- Fluoride Effects and Removal
- Mercury impact and mitigation studies
- Karst Systems and Hydrogeology
- Anaerobic Digestion and Biogas Production
- Geological and Tectonic Studies in Latin America
- Microbial metabolism and enzyme function
- Earthquake Detection and Analysis
- Atmospheric Ozone and Climate
- Reservoir Engineering and Simulation Methods
Istituto Nazionale di Geofisica e Vulcanologia
2015-2024
INGV Sezione di Palermo
2016-2024
University of Palermo
1997-2022
Terra
2008-2019
In 2011–2012, Santorini was characterized by seismic-geodetic-geochemical unrest, which unprecedented since the most-recent eruption occurred in 1950 and led to fear an imminent. This unrest offered a chance for investigating processes leading volcanic reactivation compositional characteristics of involved magma. We have thus analyzed He-Ne-Ar-isotope composition fluid inclusions olivines clinopyroxenes from cumulate mafic enclaves hosted cogenetic dacitic lavas 1570–1573 1925–1928 eruptions...
Abstract. Improving the constraints on atmospheric fate and depletion rates of acidic compounds persistently emitted by non-erupting (quiescent) volcanoes is important for quantitatively predicting environmental impact volcanic gas plumes. Here, we present new experimental data coupled with modelling studies to investigate chemical processing volcanogenic species during tropospheric dispersion. Diffusive tube samplers were deployed at Mount Etna, a very active open-conduit basaltic volcano...
Research Article| June 01, 2009 Excess methane in continental hydrothermal emissions is abiogenic Jens Fiebig; Fiebig * 1Institut für Geowissenschaften, Goethe-Universität, Altenhöferallee 1, 60438 Frankfurt am Main, Germany *E-mail: Jens.Fiebig@em.uni-frankfurt.de. Search for other works by this author on: GSW Google Scholar Alan B. Woodland; Woodland Walter D'Alessandro; D'Alessandro 2Istituto Nazionale di Geofisica e Vulcanologia, Via Ugo la Malfa 153, 90146 Palermo, Italy Wilhelm...
Starting off from a review of previous literature on kinematic models the unstable eastern flank Mt. Etna, we propose new model. The model is based our analysis large quantity multidisciplinary data deriving an extensive and diverse network INGV monitoring devices deployed along slopes volcano. Our had twofold objective: first, investigating origin recently observed slow-slip events Etna; second, defining general for instability this area To end, investigated 2008–2013 period using collected...