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件数:54件
[2014]
21.[] Permeability reduction of fractured rhyolite in volcanic conduits and its control on eruption cyclicity.[Geology,42,(2014),843-846]Satoshi Okumura, Osamu Sasaki
10.1130/G35855.1
http://www.scopus.com/inward/record.url?eid=84907285944&partnerID=40
22.[] Permeability reduction of fractured rhyolite in volcanic conduits and its control on eruption cyclicity.[Geology,42,(2014),843-846]Satoshi Okumura, Osamu Sasaki
[2013]
23.[] Carbon dioxide emission to earth's surface by deep-sea volcanism.[Geology,41,(2013),1167-1170]Satoshi Okumura, Naoto Hirano
10.1130/G34620.1
http://www.scopus.com/inward/record.url?eid=84886623662&partnerID=40
24.[] Coupled effect of magma degassing and rheology on silicic volcanism.[Earth and Planetary Science Letters,362,(2013),163-170]Satoshi Okumura, Michihiko Nakamura, Kentaro Uesugi, Tsukasa Nakano, Takuma Fujioka
10.1016/j.epsl.2012.11.056
http://www.scopus.com/inward/record.url?eid=84872194850&partnerID=40
25.[] Carbon dioxide emission to Earth’s surface by deep-sea volcanism.[Geology,(41),(2013),1167-1170]Satoshi Okumura, Naoto Hirano
26.[] Coupled effect of magma degassing and rheology on silicic volcanism.[Earth Planetary Science Letters,(2013)]Satoshi Okumura, Michihiko Nakamura, Kentaro Uesugi, Tsukasa Nakano, Takuma Fujioka
[2012]
27.[] Experimental constraints on permeable gas transport in crystalline silicic magmas.[Contributions to Mineralogy and Petrology,164,(2012),493-504]Satoshi Okumura, Michihiko Nakamura, Tsukasa Nakano, Kentaro Uesugi, Akira Tsuchiyama
10.1007/s00410-012-0750-8
http://www.scopus.com/inward/record.url?eid=84865652074&partnerID=40
28.[] 放射光X線を用いた流動するマグマのその場観察:火山噴火の多様性の原因解明へ向けて.[放射光,(2012)]奥村聡,中村美千彦,上杉健太朗
29.[] Experimental constraints on permeable gas transport in crystalline silicic magmas.[Contribution to Mineralogy and Petrology,(2012)]Satoshi Okumura, Michihiko Nakamura, Tsukasa Nakano, Kentaro Uesugi and Akira Tsuchiyama
[2011]
30.[] The H 2O content of andesitic magmas from three volcanoes in Japan, inferred from the infrared analysis of clinopyroxene.[European Journal of Mineralogy,23,(2011),771-778]Satoshi Okumura
10.1127/0935-1221/2011/0023-2141
http://www.scopus.com/inward/record.url?eid=83655197672&partnerID=40
31.[] The H2O content of andesitic magmas from three volcanoes in Japan, inferred from the infrared analysis of clinopyroxene.[The European Journal of Mineralogy,(2011)]Satoshi Okumura
[2010]
32.[] Shear deformation experiments on vesicular rhyolite: Implications for brittle fracturing, degassing, and compaction of magmas in volcanic conduits.[Journal of Geophysical Research: Solid Earth,115,(2010)]Satoshi Okumura, Michihiko Nakamura, Tsukasa Nakano, Kentaro Uesugi, Akira Tsuchiyama
10.1029/2009JB006904
http://www.scopus.com/inward/record.url?eid=77954355245&partnerID=40
33.[] Shear deformation experiments on vesicular rhyolite: Implications for brittle fracturing, degassing, and compaction of magmas in volcanic conduits.[JOURNAL OF GEOPHYSICAL RESEARCH,115(B06201),(2010)]Satoshi Okumura, Michihiko Nakamura, Tsukasa Nakano, Kentaro Uesugi, and Akira Tsuchiyama
10.1029/2009JB006904, 2010
[2009]
34.[] Magma deformation may induce non-explosive volcanism via degassing through bubble networks.[Earth and Planetary Science Letters,281,(2009),267-274]Satoshi Okumura, Michihiko Nakamura, Shingo Takeuchi, Akira Tsuchiyama, Tsukasa Nakano, Kentaro Uesugi
10.1016/j.epsl.2009.02.036
http://www.scopus.com/inward/record.url?eid=64749114480&partnerID=40
35.[] Three differentiation stages of a single magma at Piton de la Fournaise volcano (Reunion hot spot).[Geochemistry, Geophysics, Geosystems,10,(2009)]Vincent Famin, Benoît Welsch, Satoshi Okumura, Patrick Bachèlery, Satoru Nakashima
10.1029/2008GC002015
http://www.scopus.com/inward/record.url?eid=67349158678&partnerID=40
36.[] Color-change processes of a plinian pumice and experimental constraints of color-change kinetics in air of an obsidian.[Bulletin of Volcanology,71,(2009),1-13]Mihoko Moriizumi, Satoru Nakashima, Satoshi Okumura, Yuta Yamanoi
10.1007/s00445-008-0202-5
http://www.scopus.com/inward/record.url?eid=57849146840&partnerID=40
37.[] Magma deformation may induce non-explosive volcanism via degassing through connected bubbles.[Earth Planetary Science Letters,(281),(2009),267-274]Satoshi Okumura, Michihiko Nakamura, Shingo Takeuchi, Akira Tsuchiyama, Tsukasa Nakano, Kentaro Uesugi
38.[] Color change processes of a Plinian pumice and experimental constraints of color-change kinetics in air of an obsidian.[Bulletin of Volcanology,(2009)]Mihoko Moriizumi, Satoru Nakashima, Satoshi Okumura, Yuta Yamanoi
39.[] Three differentiation stages of a single magma at Piton de la Fournaise volcano (Reunion hotspot).[Geochemistry, Geophysics, Geosystems,(2009)]Vincent Famin, Benit Welsch, Satoshi Okumura, Patrick Bachelery, Satoru Nakashima
[2008]
40.[] Color measurements of volcanic ash deposits from three different styles of summit activity at Sakurajima volcano, Japan: Conduit processes recorded in color of volcanic ash.[Journal of Volcanology and Geothermal Research,178,(2008),81-93]Yuta Yamanoi, Shingo Takeuchi, Satoshi Okumura, Satoru Nakashima, Tadashi Yokoyama
10.1016/j.jvolgeores.2007.11.013
http://www.scopus.com/inward/record.url?eid=55549128570&partnerID=40
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