Zobrazeno 1 - 10
of 161
pro vyhledávání: '"Diego Perugini"'
Autor:
Marco Dionigi, Silvia Logozzo, Maria Cristina Valigi, Paola Comodi, Alessandro Pisello, Diego Perugini, Maximiliano Fastelli
Publikováno v:
Applied Sciences, Vol 14, Iss 13, p 5954 (2024)
In planetary science, visible (Vis) and near-infrared (NIR) reflectance spectra allow deciphering the chemical/mineralogical composition of celestial bodies’ surfaces by comparison between remotely acquired data and laboratory references. This pape
Externí odkaz:
https://doaj.org/article/495bbeb45bd24d4dbe66a776beb1f43d
Publikováno v:
Earth, Planets and Space, Vol 75, Iss 1, Pp 1-18 (2023)
Abstract We review pre-eruptive dynamics and evidence of open-system behavior in the volcanic plumbing system beneath Campi Flegrei Caldera, together with estimates of magma residence time, magma ascent, and mixing-to-eruption timescales. In detail,
Externí odkaz:
https://doaj.org/article/017f2f99d6a6423099060a3892d1da26
Autor:
Nicolas Bott, Rosario Brunetto, Alain Doressoundiram, Cristian Carli, Fabrizio Capaccioni, Yves Langevin, Davide Perna, François Poulet, Giovanna Serventi, Maria Sgavetti, Francesco Vetere, Diego Perugini, Cristina Pauselli, Ferenc Borondics, Christophe Sandt
Publikováno v:
Minerals, Vol 13, Iss 2, p 250 (2023)
Mercury’s peculiar orbit around the Sun (3:2 spin–orbit resonance) and lack of atmosphere result in one the widest temperature ranges experienced at the surface of a planetary body in the solar system. Temperature variations affect the physical a
Externí odkaz:
https://doaj.org/article/666f4dad5b0847e2a10d6ca84a2129cc
Autor:
Alessandro Pisello, Matteo Bisolfati, Giovanni Poggiali, Pietro Tolomei, Eleonora Braschi, John Robert Brucato, Diego Perugini
Publikováno v:
Minerals, Vol 13, Iss 2, p 170 (2023)
Volcanic products are widely present on Mercury: they occur as low-viscosity lava flows, but traces of ash deriving from explosive volcanism are also observed. Silicate glasses represent a major component in volcanic products, and it is likely that t
Externí odkaz:
https://doaj.org/article/e4ef3fa00d7f462eb16b50618ecb2554
Publikováno v:
Geosciences, Vol 12, Iss 3, p 108 (2022)
The Euganean Hills (NE Italy) magmatic district represents the final volcanic activity of the Veneto Volcanic Province. Alkaline to subalkaline magmatic suite dominated by intermediate to felsic volcanic rocks characterises the latest volcanic activi
Externí odkaz:
https://doaj.org/article/cae29b30ea3d4642ba35513053c6e467
Autor:
Ulrich Kueppers, Adriano Pimentel, Ben Ellis, Francesca Forni, Julia Neukampf, José Pacheco, Diego Perugini, Gabriela Queiroz
Publikováno v:
Frontiers in Earth Science, Vol 7 (2019)
It is well known that explosive volcanic eruptions pose serious hazards to local communities and may have worldwide impacts. However, the products of explosive eruptions on volcanic ocean islands are almost inevitably incompletely preserved as a sign
Externí odkaz:
https://doaj.org/article/f1bdb0240ca64c28975408b538893d00
Autor:
Azzurra Zucchini, Pavel N. Gavryushkin, Alexander V. Golovin, Nadezhda B. Bolotina, Paola Stabile, Michael R. Carroll, Paola Comodi, Francesco Frondini, Daniele Morgavi, Diego Perugini, Fabio Arzilli, Marco Cherin, Emmanuel Kazimoto, Konstantin Kokh, Artem Kuznetsov, Inna V. Medrish
Publikováno v:
American Mineralogist. 107:2054-2064
Carbonates in the system Na2CO3-CaCO3 are nowadays suggested as having a wide stability field at conditions of the mantle transition zone. Our structural analysis of nyerereite, which has limited stability fields at ambient conditions, and its simila
Even if silicate glasses represent a major component in volcanic products, their spectral characteristics are not always considered when dealing with the interpretation of planetary and asteroidal surfaces and terrains. Space analogues described in s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af3aa3c4f98713ea7b7b1497d1a25644
https://doi.org/10.5194/epsc2022-539
https://doi.org/10.5194/epsc2022-539
We review the evidence of open-system behavior in the volcanic plumbing system of the Campi Flegrei Caldera. Also, we highlight the estimates of magma residence time, magma ascent, and mixing-to-eruption timescales. In detail, we concentrate on the C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1c50248eef5bfc4e1e19601dc4fa2ce
https://doi.org/10.21203/rs.3.rs-1662425/v1
https://doi.org/10.21203/rs.3.rs-1662425/v1