0000000000879291

AUTHOR

M. Coltelli

showing 3 related works from this author

Insights into magma and fluid transfer at Mount Etna by a multiparametric approach: A model of the events leading to the 2011 eruptive cycle

2013

Geophysicsground deformationGeochemistry and PetrologySpace and Planetary ScienceMt. Etnavolcano plumbing systemEarth and Planetary Sciences (miscellaneous)CO2SO2CO2; ground deformation; Mt. Etna; SO2; volcanic tremor; volcano plumbing system; Geophysics; Geochemistry and Petrology; Earth and Planetary Sciences (miscellaneous); Space and Planetary Sciencevolcanic tremorCO2; ground deformation; Mt. Etna; SO2; volcanic tremor; volcano plumbing system; Geochemistry and Petrology; Geophysics; Earth and Planetary Sciences (miscellaneous); Space and Planetary Science
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Evidence of surface faulting in the archaeological site of Santa Venera al Pozzo (Catania-Eastern Sici-ly): first results from geophysical investigat…

2017

We present the first results of a preliminary geological and geophysical survey carried out in the archaeological site of Santa Venera al Pozzo (Catania, Italy). The site dates back to the Roman Age, (1st century BC). Geological surveys highlighted a set of remarkable fractures affecting some archeological remains, suggesting the occurrence of a capable fault zone through the area. Multidisciplinary geophysical surveys (seismic refraction and electrical resistivity tomographies, together with aerial photographic and thermographic survey) identified a main tectonic discontinuity ascribable to the fault zone, allowing us to infer that the fractures observed at surface could be the evidence of…

ArchaeologygeophysicSettore GEO/11 - Geofisica Applicatapaleoseismology
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Spatially resolved SO2 flux emissions from Mt Etna

2016

Abstract We report on a systematic record of SO2 flux emissions from individual vents of Etna volcano (Sicily), which we obtained using a permanent UV camera network. Observations were carried out in summer 2014, a period encompassing two eruptive episodes of the New South East Crater (NSEC) and a fissure‐fed eruption in the upper Valle del Bove. We demonstrate that our vent‐resolved SO2 flux time series allow capturing shifts in activity from one vent to another and contribute to our understanding of Etna's shallow plumbing system structure. We find that the fissure eruption contributed ~50,000 t of SO2 or ~30% of the SO2 emitted by the volcano during the 5 July to 10 August eruptive inter…

volcanic gaseGeologicalRemote Sensing and DisastersVolcanologyVolcano SeismologyVolcano MonitoringResearch LettersVolcanic GasesVolcanic Hazards and Risksvolcanic SO2 fluxSO2 camerasResearch LetterEtnaRemote Sensing of VolcanoesInstruments and TechniquesDisaster Risk Analysis and AssessmentSO2 cameraGeophysicEarth and Planetary Sciences (all)volcanic degassingNatural HazardsSeismologySolid EarthGeophysical Research Letters
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