Zobrazeno 1 - 10
of 147
pro vyhledávání: '"Marco Bonini"'
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The Mugello Basin (North-Eastern Tuscany) is an intermontane basin of the Northern Apennines (Italy) with a well-documented record of seismicity; the two major historical earthquakes occurred in 1542 (Mw = 6.0) and in 1919 (Mw = 6.4). In this study,
Externí odkaz:
https://doaj.org/article/ccaeefd8402c43778e6b35b5f0cd0ee4
Autor:
Daniele Maestrelli, Marco Bonini, Giacomo Corti, Chiara Del Ventisette, Giovanna Moratti, Domenico Montanari
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Since caldera collapse deformation is extremely difficult to study in real time - due to the high deformation rates that characterize this process and the difficult access to the caldera structures-analogue modeling has been widely used during past d
Externí odkaz:
https://doaj.org/article/0ca0b45444854f19ac0d38e289388773
Publikováno v:
Materials, Vol 10, Iss 6, p 635 (2017)
The behaviour of a granular material is mainly dependent on its frictional properties, angle of internal friction, and cohesion, which, together with material density, are the key factors to be considered during the scaling procedure of analogue mode
Externí odkaz:
https://doaj.org/article/6c148271a8ab42cea08c0e3b27a733b8
High enthalpy geothermal fields are typically associated with magmatic intrusions providing the heat source that makes the system working. To identify and locate these features, geothermal exploration generally uses expensive, time-consuming approach
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::99028221d8ad4bd20be1d377d4281687
https://doi.org/10.5194/egusphere-egu23-13667
https://doi.org/10.5194/egusphere-egu23-13667
Autor:
Daniele Maestrelli, Pietro Facincani, Federico Sani, Marco Bonini, Domenico Montanari, Chiara Del Ventisette, Giacomo Corti
Collapsed calderas are circular to elongated large depressions originating from the subsidence induced by depletion and/or migration of magma from a shallow or deep reservoir during eruptions. Despite being distributed in all tectonic settings, they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32807a0723fc47608c2978ae86a3880c
https://doi.org/10.5194/egusphere-egu23-380
https://doi.org/10.5194/egusphere-egu23-380
Autor:
Karen Nicollet, Francisco Muñoz, Geneviève Savard, Domenico Montanari, Michele d'Ambrosio, Gilberto Saccorotti, Davide Piccinini, Nicola Piana Agostinetti, Juan Luis Porras Loria, Konstantinos Michailos, Riccardo Minetto, Marco Bonini, Chiara Del Ventisette, Matteo Lupi
The Northern Apennines hinterland is normally referred to as a back-arc area affected by magmatism since the late Neogene, with intrusive and extrusive magmatic rocks being scattered through the southern Tuscany and the Tuscan Archipelago. This setti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::887f0cd8fe7ea184f5e849b97a101da1
https://doi.org/10.5194/egusphere-egu23-12965
https://doi.org/10.5194/egusphere-egu23-12965
Autor:
Cristopher López, Chiara Del Ventisette, Marco Bonini, Domenico Montanari, Daniele Maestrelli, Fernando Martínez, Rodrigo González, Rodrigo Riquelme, Daniela Montenegro, Belén Muñoz, Gabriela Guzmán‐Marusic
Publikováno v:
Tectonics. 41
Autor:
Marco Bonini, Gabriele Bicocchi, Domenico Montanari, Giovanni Ruggieri, Franco Tassi, Francesco Capecchiacci, Orlando Vaselli, Federico Sani, Daniele Maestrelli
Publikováno v:
Tectonophysics. 847:229693
Autor:
Marco Bonini
Figures S1 and S2 (normal stress changes produced by the Wenchuan and Maule earthquakes).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::323722e2e20b606b7a31f386ea927ec6
https://doi.org/10.1130/geol.s.17052392.v1
https://doi.org/10.1130/geol.s.17052392.v1