Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Heidy M Mader"'
Autor:
Fabio Arzilli, Margherita Polacci, Giuseppe La Spina, Nolwenn Le Gall, Edward W. Llewellin, Richard A. Brooker, Rafael Torres-Orozco, Danilo Di Genova, David A. Neave, Margaret E. Hartley, Heidy M. Mader, Daniele Giordano, Robert Atwood, Peter D. Lee, Florian Heidelbach, Mike R. Burton
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-14 (2022)
In situ 4D experiments at high temperature and moderate pressure reveal that rapid dendritic crystallization in hydrous basaltic magmas promotes a rheological transition within minutes, controlling magma mobility within the Earth’s crust.
Externí odkaz:
https://doaj.org/article/07c9fbea66a04e0bb559b4f74bf1599a
Autor:
Mattia Pistone, Alexia Secretan, Heidy M Mader, Paul A. Jarvis, Lukas P. Baumgartner, Jon D Blundy, Katharine V. Cashman
Publikováno v:
Crustal Magmatic System Evolution
The mixing and mingling of magmas of different compositions are important geological processes. They produce various distinctive textures and geochemical signals in both plutonic and volcanic rocks...
Autor:
Fabio Arzilli, Margherita Polacci, Giuseppe La Spina, Nolwenn Le Gall, Edward W. Llewellin, Richard A. Brooker, Rafael Torres-Orozco, Danilo Di Genova, David A. Neave, Margaret E. Hartley, Heidy M. Mader, Daniele Giordano, Robert Atwood, Peter D. Lee, Mike R. Burton
The mobility of basaltic magma within the Earth’s crust is controlled by magma viscosity. Crystallization and crystal morphology affect the viscosity, mobility and ultimately eruptibility of magma, by locking it at depth or enabling its ascent towa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de1cbeb23b3f596a8467a29be706a5a8
https://doi.org/10.5194/egusphere-egu22-5584
https://doi.org/10.5194/egusphere-egu22-5584
Autor:
Mike Burton, Edward W. Llewellin, Fabio Arzilli, Margherita Polacci, Amanda Clarke, Margaret E. Hartley, Danilo Di Genova, Mattia de' Michieli Vitturi, Heidy M Mader, Giuseppe La Spina
Basaltic volcanoes exhibit a wide range of eruptive styles, from relatively gentle effusive eruptions (producing lava flows and lava domes) to highly explosive activity (where pyroclastic materials are ejected from the vent as a jet or plume). The di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a3fd20420f78866252fd162ab08c03c
https://doi.org/10.5194/egusphere-egu21-10661
https://doi.org/10.5194/egusphere-egu21-10661
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:
Geoff Kilgour, Jon D Blundy, Stuart L. Kearns, Danilo Di Genova, Ery C. Hughes, Benjamin Buse, Heidy M Mader, Richard A. Brooker
Publikováno v:
Hughes, E C, Buse, B, Kearns, S L, Brooker, R A, Di Genova, D, Kilgour, G, Mader, H M & Blundy, J D 2020, ' The microanalysis of iron and sulphur oxidation states in silicate glass-Understanding the effects of beam damage ', IOP Conference Series: Materials Science and Engineering, vol. 891, 012014 . < https://iopscience.iop.org/article/10.1088/1757-899X/891/1/012014 >
University of Bristol-PURE
University of Bristol-PURE
Quantifying the oxidation state of multivalent elements in silicate melts (e.g., Fe2+ versus Fe3+ or S2- versus S6+) is fundamental for constraining oxygen fugacity. Oxygen fugacity is a key thermodynamic parameter in understanding melt chemical hist
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9615f1f4008cc3fde2ce33b1a50e4cd
https://resolver.caltech.edu/CaltechAUTHORS:20210226-081855287
https://resolver.caltech.edu/CaltechAUTHORS:20210226-081855287
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
Publikováno v:
Hughes, E, Buse, B, Kearns, S, Blundy, J, Kilgour, G & Mader, H 2019, ' Low analytical totals in EPMA of hydrous silicate glass due to sub-surface charging : Obtaining accurate volatiles by difference ', Chemical Geology, vol. 505, pp. 48-56 . https://doi.org/10.1016/j.chemgeo.2018.11.015
The major and minor element chemistry of silicate glass is commonly measured using electron probe micro-analysis (EPMA). The volatile content (H2O ± CO2) can, additionally, be quantified using “volatiles by difference” (VBD), but a review of lit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af349af3782c9261c02c40eca0f3545d
https://hdl.handle.net/1983/b37dff89-73ab-4c5d-9d12-017fd18f5af1
https://hdl.handle.net/1983/b37dff89-73ab-4c5d-9d12-017fd18f5af1
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/