Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Fabio L. Bonali"'
Autor:
Federico Pasquaré Mariotto, Kyriaki Drymoni, Fabio L. Bonali, Alessandro Tibaldi, Noemi Corti, Paolo Oppizzi
Publikováno v:
Resources, Vol 12, Iss 2, p 29 (2023)
This work is aimed at reviewing the current state of the art in geosite selection, assessment, and communication. We first highlight the main papers that have defined paramount concepts such as geodiversity, geoheritage, and geosites. We then delve i
Externí odkaz:
https://doaj.org/article/27ab0574c9c94ddba96f6b7ebbabd21f
Autor:
Fabio L. Bonali, Elena Russo, Fabio Vitello, Varvara Antoniou, Fabio Marchese, Luca Fallati, Valentina Bracchi, Noemi Corti, Alessandra Savini, Malcolm Whitworth, Kyriaki Drymoni, Federico Pasquaré Mariotto, Paraskevi Nomikou, Eva Sciacca, Sofia Bressan, Susanna Falsaperla, Danilo Reitano, Benjamin van Wyk de Vries, Mel Krokos, Giuliana Panieri, Mathew Alexander Stiller-Reeve, Giuseppe Vizzari, Ugo Becciani, Alessandro Tibaldi
Publikováno v:
Geosciences, Vol 12, Iss 1, p 9 (2021)
Immersive virtual reality can potentially open up interesting geological sites to students, academics and others who may not have had the opportunity to visit such sites previously. We study how users perceive the usefulness of an immersive virtual r
Externí odkaz:
https://doaj.org/article/409096e6e6c24b09b0fd302d4e16ad0d
Autor:
Noemi Corti, Fabio L. Bonali, Federico Pasquaré Mariotto, Alessandro Tibaldi, Elena Russo, Ásta Rut Hjartardóttir, Páll Einarsson, Valentina Rigoni, Sofia Bressan
Publikováno v:
Geosciences, Vol 11, Iss 2, p 101 (2021)
In the Northern Volcanic Zone of Iceland, the geometry, kinematics and offset amount of the structures that form the active Krafla Rift were studied. This rift is composed of a central volcano and a swarm of extension fractures, normal faults and eru
Externí odkaz:
https://doaj.org/article/ea54fe1593974b09a4ac0b62eea27519
Autor:
Alessandro Tibaldi, Fabio L. Bonali, Noemi Corti, Elena Russo, Kyriaki Drymoni, Emanuela De Beni, Stefano Branca, Marco Neri, Massimo Cantarero, Federico Pasquarè Mariotto
Publikováno v:
Tectonophysics. 837:229468
The 1928 CE volcanic activity on eastern Etna, Italy, produced wide surface deformation and high effusion rates along fissures, with excess volumes of about 50 million m3 of lavas. This, in conjunction with the low elevation of the main eruptive vent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f3a7defc29c0f30fc340b46218761b55
https://doi.org/10.1016/j.tecto.2022.229468
https://doi.org/10.1016/j.tecto.2022.229468