Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Vicky Hards"'
Publikováno v:
Journal of the Geological Society, 2015, Vol.172(4), pp.533-539 [Peer Reviewed Journal]
The recent study by Devine & Rutherford (2014), ‘Magma storage region processes of the Soufriere Hills Volcano, Montserrat’, published as Chapter 19 of the Geological Society of London Memoir, Volume 39, focused primarily on updating the record o
Autor:
G. Wadge, T. Christopher, B. Taisne, Marie Edmonds, Vicky Hards, Henry M. Odbert, Antonio Costa
Publikováno v:
Geological Society, London, Special Publications
Soufriere Hills Volcano produced prodigious quantities of sulphur dioxide (SO2) gas throughout 1995–2013. An unprecedented, detailed record of SO2 flux shows that high SO2 fluxes were sustained through eruptive pauses and for two years after the en
The Soufrière Hills Volcano in Montserrat erupts a Cl-rich, porphyritic andesite. HCl degassing accompanies eruption and is dependent on the growth rate of the lava dome. The magma contains hornblende phenocrysts that show repetitive zoning in most
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dfd837b064f84d29274e26908b303fe
https://ora.ox.ac.uk/objects/uuid:b666c441-3b05-49ac-ab1a-148bca0bfcf6
https://ora.ox.ac.uk/objects/uuid:b666c441-3b05-49ac-ab1a-148bca0bfcf6
The Soufrière Hills volcano on Montserrat has for the past 12 years been erupting andesite with basaltic to basaltic-andesite inclusions. The andesite contains a wide variety of phenocryst textures and strongly zoned microlites. Analysis of minor el
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61620ba1a0147bc01dc54fca57548293
https://ora.ox.ac.uk/objects/uuid:6bb8e90e-bb04-45f6-8e57-457078c5e44a
https://ora.ox.ac.uk/objects/uuid:6bb8e90e-bb04-45f6-8e57-457078c5e44a
Autor:
L. A. Rodriguez, Marie Edmonds, Clive Oppenheimer, G. Ryan, I. Matthew Watson, Vicky Hards, Gregg J. S. Bluth
Publikováno v:
Journal of Volcanology and Geothermal Research. 173:135-147
To improve interpretation of volcanic SO2 flux data, it is necessary to quantify and understand reactions involving SO2 in volcanic plumes. SO2 is lost in volcanic plumes through a number of mechanisms. Here we report SO2 measurements made with minia
Publikováno v:
Energy. 32:1194-1201
Carbon dioxide (CO2) capture and storage has the potential to reduce CO2 emissions from fossil fuel combustion. Although leakage from monitored CO2 injection sites has been minimal to non-existent, experience from the natural gas storage industry sug
Autor:
Vicky Hards, Geoff Nowell, P.M. Antoshechkina, V. Niku-Paavola, Robert N. Thompson, Alan P. Dickin, D.G. Pearson, Chris J. Ottley, A. J. V. Riches, A.-K. Nguno
Publikováno v:
Journal of Petrology. 48:1119-1154
Early Cretaceous tholeiitic picrite-to-rhyolite dykes around Spitzkoppe, western Namibia, are part of the extensive Henties Bay–Outjo swarm, penecontemporaneous with 132 Ma Etendeka lavas 100 km to the NW. Although only intermediate to rhyolitic dy
Autor:
T. Christopher, M.H. Strutt, S. De Angelis, Vicky Hards, G. Ryan, Susan C. Loughlin, Lee Jones, R. Luckett
Publikováno v:
Geophysical Research Letters. 37
[1] The third episode of lava dome growth at Soufriere Hills Volcano, Montserrat was characterised by higher average magma discharge rates than either previous dome growth episode at this volcano and yet fewer collapses. During sustained dome growth
Publikováno v:
Geophysical Research Letters. 37
Arc volcanoes commonly show evidence of mixing between mafic and silicic magma. Melt inclusions and matrix glasses in andesite erupted from Soufriere Hills Volcano, Montserrat, include an anomalously K2O-rich population which shows close compositiona
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 7, Iss 4, Pp 467-472 (2007)
Scopus-Elsevier
Natural Hazards and Earth System Sciences
Natural Hazards and Earth System Sciences, Copernicus Publ. / European Geosciences Union, 2007, 7 (4), pp.467-472
Scopus-Elsevier
Natural Hazards and Earth System Sciences
Natural Hazards and Earth System Sciences, Copernicus Publ. / European Geosciences Union, 2007, 7 (4), pp.467-472
A partial dome collapse with concurrent pyroclastic flow (PF) activity occurred at Soufrière Hills Volcano (SHV), Montserrat on 8 January 2007. Pyroclastic density currents were observed to propagate from the Northwest and West sectors of the summit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::afcb20d7c7c93d0f5182355487c906e1
http://www.nat-hazards-earth-syst-sci.net/7/467/2007/nhess-7-467-2007.html
http://www.nat-hazards-earth-syst-sci.net/7/467/2007/nhess-7-467-2007.html