Zobrazeno 1 - 10
of 27
pro vyhledávání: '"DI NAPOLI, Rossella"'
Autor:
Aiuppa, Alessandro, Fischer, Tobias P., Plank, Terry, Robidoux, Philippe, Di Napoli, Rossella
Publikováno v:
In Earth-Science Reviews May 2017 168:24-47
Autor:
Di Napoli, Rossella, Aiuppa, Alessandro, Bergsson, Baldur, Ilyinskaya, Evgenia, Pfeffer, Melissa Anne, Guðjónsdóttir, Sylvía Rakel, Valenza, Mariano
Publikováno v:
In Chemical Geology 20 January 2016 420:251-269
Autor:
Allard, Patrick, Aiuppa, Alessandro, Beauducel, François, Gaudin, Damien, Di Napoli, Rossella, Calabrese, Sergio, Parello, Francesco, Crispi, Olivier, Hammouya, Gilbert, Tamburello, Giancarlo
Publikováno v:
In Chemical Geology 25 September 2014 384:76-93
Autor:
Allard, P, AIUPPA, Alessandro, Beauducel, F, CALABRESE, Sergio, DI NAPOLI, Rossella, Crispi, O, Gaudin, D, PARELLO, Francesco, Hammouya, G, TAMBURELLO, Giancarlo
Since its last magmatic eruption in 1530 AD, La Soufrière andesitic volcano in Guadeloupe has displayed intense hydrothermal activity and six phreatic eruptive crises (the last of which, in 1976-1977, with 73000 evacuees). Here we report on the firs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::b8705cd04c6593cf904db007804c4bd5
http://hdl.handle.net/10447/143742
http://hdl.handle.net/10447/143742
Autor:
AIUPPA, Alessandro, TAMBURELLO, Giancarlo, DI NAPOLI, Rossella, Liuzzo,M, Giudice, G, Bergsson, B, Ilyinskaya,E, Papazachos, C, Vougioukalakis, G, Francofonte, V.
The Multi-component Gas Analyzer System (Multi-GAS) has recently consolidated as a standard technique for the nearly real-time in-situ observation of major volcanogenic components (H2O, CO2, SO2, H2S,H2) in volcanic gas plumes. The Multi-GAS has been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::dbdf64f4428f4b92196184ea8317078e
http://hdl.handle.net/10447/97814
http://hdl.handle.net/10447/97814
Autor:
Aiuppa, Alessandro, Tamburello, Giancarlo, Di Napoli, Rossella, Cardellini, Carlo, Chiodini, Giovanni, Giudice, Gaetano, Grassa, Fausto, Pedone, Maria
Publikováno v:
Geochemistry, Geophysics, Geosystems
The fumarolic gas output has not been quantified for any of the currently deforming calderas worldwide, due to the lack of suitable gas flux sensing techniques. In view of resumption of ground uplift (since 2005) and the associated variations in gas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::298c4db9f31d82752975e8e36fd9c9f9
Autor:
AIUPPA, Alessandro, DI NAPOLI, Rossella, PEDONE, Maria, TAMBURELLO, Giancarlo, Allard, P, Beauducel,F, Cardellini,C, Chiodini, G, Federico,C, Gaudin, D, Giudice,G, Grassa, F
Quantifying the flux of magma derived CO2 dissipated by fumarolic fields at dormant volcanoes is fundamental to assess their current state of hydrothermal activity and, therefore, the likelihood of a future phreatic/magmatic eruption. There is, in fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::b73772c271e0f57097ba8034d1209bfb
http://hdl.handle.net/10447/96609
http://hdl.handle.net/10447/96609
Hydrothermal systems hosted within active volcanic systems represent an excellent opportunity to investigate the interactions between aquifer rocks, infiltrating waters and deep-rising magmatic fluids, and thus allow deriving information on the activ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::f535caa1bdd73fa172852add3e8e47cb
http://hdl.handle.net/10447/66552
http://hdl.handle.net/10447/66552
Autor:
DI NAPOLI, Rossella, AIUPPA, Alessandro, PARELLO, Francesco, CALABRESE, Sergio, VALENZA, Mariano, Fourré, E, Jean Baptiste, P, Allard, P, Gaubi, E, Ben Mamou, A
Tunisia is characterized by hot and warm groundwaters (temperature up to 75 °C) which represent the surface manifestation of geothermal systems hosted in carbonate-evaporite rock sequences. The T-conditions of Tunisia deep thermal reservoirs are her
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::1b95ee1e7f6143289b99c181407cb85a
http://hdl.handle.net/10447/72279
http://hdl.handle.net/10447/72279
Dominica, a small Caribbean island between Martinique (to the South) and Guadeloupe (to the North), is, because of the high number of potentially active volcanic centres,one of the most susceptible sites to volcanic risk in the Lesser Antilles arc. S
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3658::973731a9df46a5d403385c84299ed088
http://hdl.handle.net/10447/72283
http://hdl.handle.net/10447/72283