Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Alex Scarani"'
Autor:
Alex Scarani, Alessio Zandonà, Fabrizio Di Fiore, Pedro Valdivia, Rizaldi Putra, Nobuyoshi Miyajima, Hansjörg Bornhöft, Alessandro Vona, Joachim Deubener, Claudia Romano, Danilo Di Genova
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-14 (2022)
Nanocrystallization in experiments on basalt melts and glasses from Mt. Etna and Stromboli is mainly triggered by undercooling-driven oversaturation in TiO2 and FeO, which could bias viscosity measurements and affect magma dynamics during decompressi
Externí odkaz:
https://doaj.org/article/2d5672364f7e4bdf8b762832a2865254
Autor:
János Szepesi, Alessandro Vona, István János Kovács, Krisztián Fintor, Kata Molnár, Alex Scarani, Guido Giordano, Réka Lukács
The silicic flows and domes can impose mechanical and thermal stress on the underlying substrate causing mineralization and lithification of granular bodies. In addition, the released water from the permeable substrate as dominant volatile species ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::682ec2c648d1f032e3c79b895f9995c9
https://doi.org/10.5194/egusphere-egu23-12320
https://doi.org/10.5194/egusphere-egu23-12320
Autor:
Fabrizio Di Fiore, Alessandro Vona, Alex Scarani, Guido Giordano, Claudia Romano, Daniele Giordano, Luca Caricchi, Alba Martin-Lorenzo, Fatima Rodriguez, Beverley Coldwell, Pedro Hernandez, Matt Pankhurst
After half a century of quiescence, activity at Cumbre Vieja volcano (La Palma, Canary Islands, Spain) restarted with a spectacular flank eruption characterized by both high fire fountaining and effusive activity. The products emitted comprise tephra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f02946d0aae5279dd611df8d91d4b67
https://doi.org/10.5194/egusphere-egu22-11700
https://doi.org/10.5194/egusphere-egu22-11700
Autor:
Alex Scarani, Alessandro Vona, Danilo Di Genova, Raschid Al-Mukadam, Claudia Romano, Joachim Deubener
Publikováno v:
Contributions to Mineralogy and Petrology. 177
Volcanic materials can experience up to eleven orders of magnitude of cooling rate (qc) starting from 10–5 K s−1. The glassy component of volcanic material is routinely measured via differential scanning calorimeter (DSC) to obtain qc through the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c4de5d5acbe9a671c5ed8d430679cb4a
https://doi.org/10.1007/s00410-022-01899-5
https://doi.org/10.1007/s00410-022-01899-5