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Marcello Martini

Researcher at National Institute of Geophysics and Volcanology

Publications -  87
Citations -  3106

Marcello Martini is an academic researcher from National Institute of Geophysics and Volcanology. The author has contributed to research in topics: Volcano & Caldera. The author has an hindex of 27, co-authored 87 publications receiving 2808 citations.

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Source mechanisms of explosions at Stromboli Volcano, Italy, determined from moment-tensor inversions of very-long-period data

TL;DR: In this article, two source centroids are identified, each representative of the distinct event types associated with explosive eruptions from two different vents, and the two sources that best fit the data are offset 220 and 260 m beneath and 160 m northwest of the active vents, respectively.
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Source and path effects in the wave fields of tremor and explosions at Stromboli Volcano, Italy

TL;DR: In this paper, the authors investigated the wave fields generated by Strombolian activity using data from small-aperture seismic arrays deployed on the north flank of Stromboli and data from seismic and pressure transducers set up near the summit crater.
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Automatic Classification of Seismic Signals at Mt. Vesuvius Volcano, Italy, Using Neural Networks

TL;DR: A new strategy for reliable automatic classification of local seismic signals and volcano-tectonic earthquakes (vt) is presented, based on a supervised neural network in which a new approach for feature extraction from short period seismic signals is applied.
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Repeated fluid‐transfer episodes as a mechanism for the recent dynamics of Campi Flegrei caldera (1989–2010)

TL;DR: In this paper, the authors analyzed a multiparametric data set of seismological, geodetic and geochemical data recorded at Campi Flegrei caldera since 1982.
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Magma injection beneath the urban area of Naples: a new mechanism for the 2012-2013 volcanic unrest at Campi Flegrei caldera

TL;DR: The first evidence, in the last 30 years, of a renewed magmatic activity at Campi Flegrei caldera from January 2012 to June 2013 is found, and has implications on the evaluation of the volcanic risk and in the volcanic surveillance of this densely populated area.