Fabio Ferri
University of Padua
17 Papers
45 Citations
Fabio Ferri is an academic researcher from University of Padua. The author has contributed to research in topics: Fluid inclusions & Slip (materials science). The author has an hindex of 9, co-authored 16 publications. Previous affiliations of Fabio Ferri include University of Los Andes.
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Papers
Low- to high-velocity frictional properties of the clay-rich gouges from the slipping zone of the 1963 Vaiont slide, northern Italy
Fabio Ferri,Giulio Di Toro,Giulio Di Toro,Takehiro Hirose,Raehee Han,Hiroyuki Noda,Toshihiko Shimamoto,Marino Quaresimin,Nicola De Rossi +8 more
TL;DR: In this article, the authors investigated the frictional properties of the clay-rich layers under similar deformation conditions as during the 1963 Vaiont landslide: 1.5 MPa normal stress, 2 × 10^(−7) to 1.31 m/s slip rate and displacements up to 34 m.
Seismic properties of lower crustal xenoliths from El Hoyazo (SE Spain): Experimental evidence up to partial melting
TL;DR: In this article, the authors measured compressional wave velocities up to conditions exceeding the beginning of melting (950°C at 500MPa confining pressure) on three garnet-biotite-sillimanite metapelitic xenoliths recovered from the Neogene dacites of El Hoyazo (SE Spain).
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An Experimental Determination of the Effect of Bulk Composition on Phase Relationships in Metasediments at Near-solidus Conditions
TL;DR: The evolution of metapelites and metagreywackescan can be reconstructed if the dependence of phase relationships on pressure, temperature and bulk composition is well known as mentioned in this paper.
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Electrical conductivity in a partially molten crust from measurements on metasedimentary enclaves
TL;DR: In this paper, the complex electrical impedance of a garnet-biotite-sillimanite residual enclave in the Neogene dacite of El Hoyazo (SE Spain) has been determined up to 978-°C at 200-300 MPa.
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Melt inclusions in arclogitic xenoliths constrain the genesis of the lower continental arc crust beneath the Northern Volcanic Zone, Colombia
Omar Gianola,Fabio Ferri,Mattia Gilio,Maurizio Petrelli,Mara Murri,Anna Barbaro,Matteo Alvaro,Stefano Poli,Bernardo Cesare +8 more
TL;DR: In this paper , pressure and temperature conditions for the studied arclogites were estimated by intracrystalline geothermometry, elastic geometry, phase equilibria modelling and classical Fe-Mg exchange between garnet and clinopyroxene.
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