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P. Mario Nuccio

Researcher at University of Palermo

Publications -  5
Citations -  230

P. Mario Nuccio is an academic researcher from University of Palermo. The author has contributed to research in topics: Chondrite & Volcano. The author has an hindex of 4, co-authored 5 publications receiving 214 citations. Previous affiliations of P. Mario Nuccio include National Institute of Geophysics and Volcanology.

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Geochemical evidence of melt intrusions along lithospheric faults of the Southern Apennines, Italy: Geodynamic and seismogenic implications

TL;DR: In this paper, the authors investigated gas emissions in the Southern Apennine axial zone of the Adriatic plate and found that CO2 emissions are generally CO2-dominated, have 3He/4He ratios in the range of 0.09-2.84 Ra, and display both 3He and 4He outputs in the ranges of those reported for the Italian active volcanoes Phlegrean Fields and Vulcano.
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Evidence of deep magma degassing and ascent by geochemistry of peripheral gas emissions at Mount Etna (Italy): Assessment of the magmatic reservoir pressure

TL;DR: In this article, the initial and final pressures of the magma batches feeding the emissions were computed based on numerical simulations of volatile degassing from Etnean basalts, which can define the levels of the Etna plumbing system where magmas are stored.
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Remote detection of fumarolic gas chemistry at Vulcano, Italy, using an FT-IR spectral radiometer

TL;DR: In this article, an infrared absorption spectroscopy remote sensing technique was used to determine the SO 2 /HCl ratio in fumarolic plumes at Vulcano, Italy.
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Gas hazard assessment at the Monticchio crater lakes of Mt. Vulture, a volcano in Southern Italy

TL;DR: In this paper, the authors have shown that there is a considerable inflow of gas into both crater lakes of Monticchio, Southern Italy, which are located in two maars that formed 140, 000 years ago during Mt. Vulture volcano last eruptive activity.
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Piancaldoli meteorite: chemistry, mineralogy and petrology

TL;DR: The Piancaldoli meteorite was found on the roof of a house in Florence, Italy in 1968 as mentioned in this paper, and the trajectory and the terminal point were calculated, leading to the recovery of three small meteoritic fragments.