Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Emily C. Bamber"'
Autor:
Emily C. Bamber, Giuseppe La Spina, Fabio Arzilli, Margherita Polacci, Lucia Mancini, Mattia de’ Michieli Vitturi, Daniele Andronico, Rosa Anna Corsaro, Mike R. Burton
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-16 (2024)
Abstract Explosivity of basaltic eruptions is related to the efficiency in which exsolved gas can separate from the melt during ascent, which is controlled by magma permeability. However, basaltic pyroclasts from eruptions of varying explosivity can
Externí odkaz:
https://doaj.org/article/8d8ec7b33698489daaa926898f741b57
Autor:
Emily C. Bamber, Giuseppe La Spina, Fabio Arzilli, Mattia de’ Michieli Vitturi, Margherita Polacci, Margaret E. Hartley, Maurizio Petrelli, Jonathan Fellowes, Mike Burton
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-17 (2022)
Large explosive eruptions of basaltic magma are promoted by low pre-eruptive temperatures in crystallising shallow magma reservoirs, according to an integrated petrological, geochemical and numerical modelling study.
Externí odkaz:
https://doaj.org/article/68c2de1f9c5341869d65196e54b843b2
Autor:
Mike Burton, Margherita Polacci, Margaret E. Hartley, José Armando Saballos, Maurizio Petrelli, Mattia de' Michieli Vitturi, Giuseppe La Spina, Fabio Arzilli, Emily C. Bamber, David Chavarría, Jonathan Fellowes
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Richard A. Brooker, Joachim Deubener, Louis Hennet, Simone Anzellini, Sara Fanara, Allessandro Longo, Heidy M Mader, Giuseppe La Spina, Olga Shebanova, Nobuyoshi Miyajima, Daniel R. Neuville, Danilo Di Genova, Fabio Arzilli, James W E Drewitt, Emily C. Bamber
Publikováno v:
Science Advances
Science Advances, American Association for the Advancement of Science (AAAS), 2020, 6 (39), pp.eabb0413. ⟨10.1126/sciadv.abb0413⟩
Di Genova, D, Brooker, R A, Mader, H M, Drewitt, J W E, Longo, A, Deubener, J, Neuville, D R, Fanara, S, Shebanova, O, Anzellini, S, Arzilli, F, Bamber, E C, Hennet, L, La Spina, G & Miyajima, N 2020, ' In situ observation of nanolite growth in volcanic melt : A driving force for explosive eruptions ', Science Advances, vol. 6, no. 39, eabb0413 . https://doi.org/10.1126/sciadv.abb0413
Di Genova, D, Brooker, R A, Mader, H M, Drewitt, J W E, Longo, A, Deubener, J, Neuville, D R, Fanara, S, Shebanova, O, Anzellini, S, Arzilli, F, Bamber, E C, Hennet, L, La Spina, G & Miyajima, N 2020, ' In situ observation of nanolite growth in volcanic melt : a driving force for explosive eruptions ', Science Advances, vol. 6, no. 39, eabb0413 . https://doi.org/10.1126/sciadv.abb0413
'Science Advances ', vol: 6, pages: eabb0413-1-eabb0413-14 (2020)
Science Advances, American Association for the Advancement of Science (AAAS), 2020, 6 (39), pp.eabb0413. ⟨10.1126/sciadv.abb0413⟩
Di Genova, D, Brooker, R A, Mader, H M, Drewitt, J W E, Longo, A, Deubener, J, Neuville, D R, Fanara, S, Shebanova, O, Anzellini, S, Arzilli, F, Bamber, E C, Hennet, L, La Spina, G & Miyajima, N 2020, ' In situ observation of nanolite growth in volcanic melt : A driving force for explosive eruptions ', Science Advances, vol. 6, no. 39, eabb0413 . https://doi.org/10.1126/sciadv.abb0413
Di Genova, D, Brooker, R A, Mader, H M, Drewitt, J W E, Longo, A, Deubener, J, Neuville, D R, Fanara, S, Shebanova, O, Anzellini, S, Arzilli, F, Bamber, E C, Hennet, L, La Spina, G & Miyajima, N 2020, ' In situ observation of nanolite growth in volcanic melt : a driving force for explosive eruptions ', Science Advances, vol. 6, no. 39, eabb0413 . https://doi.org/10.1126/sciadv.abb0413
'Science Advances ', vol: 6, pages: eabb0413-1-eabb0413-14 (2020)
This study shows how a few nanometer-sized crystals markedly increase the viscosity of a magma leading to explosive eruptions.
Although gas exsolution is a major driving force behind explosive volcanic eruptions, viscosity is critical in control
Although gas exsolution is a major driving force behind explosive volcanic eruptions, viscosity is critical in control
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e8fe2813b83ef891b5cddf863f815442
https://hal.archives-ouvertes.fr/hal-02948125
https://hal.archives-ouvertes.fr/hal-02948125
Autor:
Fabio Arzilli, Emily C. Bamber, Mattia de' Michieli Vitturi, Margherita Polacci, Mike Burton, Margaret E. Hartley, José Armando Saballos, Giuseppe La Spina, David Chavarría, Jonathan Fellowes, Maurizio Petrelli, Danilo Di Genova
Plinian eruptions are the most hazardous yet enigmatic style of volcanism at basaltic systems. The low viscosity of basaltic magma should preclude its fragmentation; however, there are several recognised examples of basaltic Plinian activity. Histori
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d50554733ec7f90df882c184ff140601
https://doi.org/10.5194/egusphere-egu2020-9513
https://doi.org/10.5194/egusphere-egu2020-9513
Autor:
Nolwenn Le Gall, Nghia T. Vo, Sara Nonni, Mike Burton, Peter D. Lee, Biao Cai, Danilo Di Genova, Emily C. Bamber, Richard A. Brooker, Margherita Polacci, Edward W. Llewellin, Fabio Arzilli, Margaret E. Hartley, Heidy M Mader, Giuseppe La Spina, Robert C. Atwood
Publikováno v:
Goldschmidt Abstracts.
Basaltic eruptions are the most common form of volcanism on Earth and planetary bodies. The low viscosity of basaltic magmas generally favours effusive and mildly explosive volcanic activity. Highly explosive basaltic eruptions occur less frequently
Autor:
Sara Nonni, Nolwenn Le Gall, Peter D. Lee, Fabio Arzilli, Mike Burton, Edward W. Llewellin, Margherita Polacci, Margaret E. Hartley, Emily C. Bamber, Robert C. Atwood, Danilo Di Genova, Nghia T. Vo, Biao Cai, Heidy M Mader, Giuseppe La Spina, Richard A. Brooker
Publikováno v:
Geoscience, 2019, Vol.12, pp.1023-1028 [Peer Reviewed Journal]
Arzilli, F, La Spina, G, Burton, M, Polacci, M, Le Gall, N, Hartley, M, Genova, D D, Cai, B, Vo, N T, Bamber, E, Nonni, S, Atwood, R, Llewellin, E W, Brooker, R A, Mader, H M & Lee, P D 2019, ' Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallisation ', Nature Geoscience, vol. 12, pp. 1023-1028 . https://doi.org/10.1038/s41561-019-0468-6
Arzilli, F, La Spina, G, Burton, M, Polacci, M, Le Gall, N, Hartley, M, Di Genova, D, Cai, B, Vo, N, Bamber, E, Nonni, S, Atwood, R, Llewellin, E, Brooker, R, Mader, H & Lee, P 2019, ' Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallisation ', Nature Geoscience, vol. 12, pp. 1023–1028 . https://doi.org/10.1038/s41561-019-0468-6
Arzilli, F, La Spina, G, Burton, M, Polacci, M, Le Gall, N, Hartley, M, Genova, D D, Cai, B, Vo, N T, Bamber, E, Nonni, S, Atwood, R, Llewellin, E W, Brooker, R A, Mader, H M & Lee, P D 2019, ' Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallisation ', Nature Geoscience, vol. 12, pp. 1023-1028 . https://doi.org/10.1038/s41561-019-0468-6
Arzilli, F, La Spina, G, Burton, M, Polacci, M, Le Gall, N, Hartley, M, Di Genova, D, Cai, B, Vo, N, Bamber, E, Nonni, S, Atwood, R, Llewellin, E, Brooker, R, Mader, H & Lee, P 2019, ' Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallisation ', Nature Geoscience, vol. 12, pp. 1023–1028 . https://doi.org/10.1038/s41561-019-0468-6
Basaltic eruptions are the most common form of volcanism on Earth and planetary bodies. The low viscosity of basaltic magmas inhibits fragmentation, which favours effusive and lava-fountaining activity, yet highly explosive, hazardous basaltic erupti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c35af8756dff3b0eace9df5a3c123c5a
http://dro.dur.ac.uk/29181/
http://dro.dur.ac.uk/29181/