Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Olivier Reubi"'
Autor:
Olivier Reubi, Othmar Müntener
Publikováno v:
Journal of Petrology. 63
Andesites are iconic of subduction zone magmatism. Yet intermediate magmas (57–66 wt % SiO2) are less abundant than generally thought in arc settings. A comparison of experimental hydrous liquid lines of descent, melt inclusions and bulk-rock compo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f785071e8db74b69f641ac96d6de695
https://doi.org/10.1093/petrology/egac044
https://doi.org/10.1093/petrology/egac044
Publikováno v:
Journal of Petrology. 58:261-276
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::552d0fa5117a9015e42677980325dd91
https://doi.org/10.1093/petrology/egx015
https://doi.org/10.1093/petrology/egx015
Publikováno v:
Volcán de Colima ISBN: 9783642259104
Volcan de Colima’s nearly continuous activity since 1998 has shifted repeatedly from effusive to explosive Vulcanian eruptions. Strong explosions occurred in 1999 and 2005, which raised concerns that the current eruptive phase may lead to a major P
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb08ef8bc16df3916fb680eb452f7f4f
https://doi.org/10.1007/978-3-642-25911-1_9
https://doi.org/10.1007/978-3-642-25911-1_9
Autor:
Olivier Reubi, Jon D Blundy
Publikováno v:
Nature. 461:1269-1273
Andesites represent a large proportion of the magmas erupted at continental arc volcanoes and are regarded as a major component in the formation of continental crust. Andesite petrogenesis is therefore fundamental in terms of both volcanic hazard and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a35dff9f1e596f50411bc3788a9d0fe
https://doi.org/10.1038/nature08510
https://doi.org/10.1038/nature08510
Autor:
Jon D Blundy, Olivier Reubi
Publikováno v:
Journal of Petrology. 49:2221-2243
Phenocryst-hosted melt inclusions from the 1998^2005 andesite eruptions of Volcan de Colima (Mexico) show broad ranges of major and trace element contents that do not overlap with the bulk- rock compositions and indicate that melt inclusions can be f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0108937983460dcc825b02cd2737f9d6
https://doi.org/10.1093/petrology/egn066
https://doi.org/10.1093/petrology/egn066
Autor:
Olivier Reubi, Ian Angus Nicholls
Publikováno v:
Journal of Petrology. 46:1367-1391
The Batur volcanic field (BVF), in Bali, Indonesia, underwent two successive caldera-forming eruptions that resulted in the deposition of silicic ignimbrites. The magmas erupted during and between these eruptions show a broad range of compositions fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::881e5fe428e68bfacc54a271d61ad2b4
https://doi.org/10.1093/petrology/egi019
https://doi.org/10.1093/petrology/egi019
Autor:
Olivier Reubi, Ian Angus Nicholls
Publikováno v:
Journal of Volcanology and Geothermal Research. 138:345-369
Batur volcanic field (BVF), in Bali, Indonesia underwent a complex evolution that comprised three periods of building and two major caldera-forming eruptions. The magmas erupted show a broad range of compositions from basaltic to rhyolitic (50–71 w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1856de07c50bbb716495fe94c79b307a
https://doi.org/10.1016/j.jvolgeores.2004.07.009
https://doi.org/10.1016/j.jvolgeores.2004.07.009
Autor:
Olivier Reubi, Ian Angus Nicholls
Publikováno v:
Bulletin of Volcanology. 66:134-148
Batur volcanic field (BVF) in Bali, Indonesia, underwent two successive caldera-forming eruptions, CI and CII (29,300 and 20,150 years b.p., respectively) that resulted in the deposition of dacitic ignimbrites. The respective ignimbrites show contras
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11f4e2fe3c0a15b0fa69b9b6d681b47f
https://doi.org/10.1007/s00445-003-0298-6
https://doi.org/10.1007/s00445-003-0298-6
Publikováno v:
Geological Society of America Bulletin. 117:1615
An up-to-180-m-thick debris avalanche deposit related to Ferrar large igneous province magmatism is observed at central Allan Hills, Antarctica. This Jurassic debris avalanche deposit forms the lower part (member m 1 ) of the Mawson Formation and is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88e9e67bd23dea6c27a1a38625920b6f
https://doi.org/10.1130/b25766.1
https://doi.org/10.1130/b25766.1
Autor:
Olivier Reubi, Jon Blundy
Publikováno v:
Journal of Petrology; Dec2008, Vol. 49 Issue 12, p2221-2221, 1p