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Mashima, Hidehisa (2009) The basalt-high magnesium andesite association formed by multi-stage partial melting of a heterogeneous source mantle: Evidence from Hirado-Seto, Northwest Kyushu, Southwest Japan. Lithos, 112 (3) 351-366 doi:10.1016/j.lithos.2009.03.016

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Reference TypeJournal (article/letter/editorial)
TitleThe basalt-high magnesium andesite association formed by multi-stage partial melting of a heterogeneous source mantle: Evidence from Hirado-Seto, Northwest Kyushu, Southwest Japan
JournalLithos
AuthorsMashima, HidehisaAuthor
Year2009 (October)Volume112
Issue3
PublisherElsevier BV
DOIdoi:10.1016/j.lithos.2009.03.016Search in ResearchGate
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Mindat Ref. ID271936Long-form Identifiermindat:1:5:271936:2
GUID0
Full ReferenceMashima, Hidehisa (2009) The basalt-high magnesium andesite association formed by multi-stage partial melting of a heterogeneous source mantle: Evidence from Hirado-Seto, Northwest Kyushu, Southwest Japan. Lithos, 112 (3) 351-366 doi:10.1016/j.lithos.2009.03.016
Plain TextMashima, Hidehisa (2009) The basalt-high magnesium andesite association formed by multi-stage partial melting of a heterogeneous source mantle: Evidence from Hirado-Seto, Northwest Kyushu, Southwest Japan. Lithos, 112 (3) 351-366 doi:10.1016/j.lithos.2009.03.016
In(2009, October) Lithos Vol. 112 (3) Elsevier BV

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Kamei, Atsushi, Miyake, Yasuyuki, Owada, Masaaki, Kimura, Jun-Ichi (2009) A pseudo adakite derived from partial melting of tonalitic to granodioritic crust, Kyushu, southwest Japan arc. Lithos, 112 (3) 615-625 doi:10.1016/j.lithos.2009.05.024
Mashima, Hidehisa (2009) A melting anomaly in Northwest Kyushu, Southwest Japan: A consequence of the tectonic evolution of NW Kyushu and the origin of a pseudo hot spot in a convergent zone. Journal of Volcanology and Geothermal Research, 186 (3) 195-209 doi:10.1016/j.jvolgeores.2009.06.008
Mashima, Hidehisa (2005) Partial melting controls on the northwest Kyushu basalts from Saga-Futagoyama. The Island Arc, 14 (2). 165-177 doi:10.1111/j.1440-1738.2005.00466.x
Mashima, Hidehisa (2004) Time scale of magma mixing between basalt and dacite estimated for the Saga–Futagoyama volcanic rocks in northwest Kyushu, southwest Japan. Journal of Volcanology and Geothermal Research, 131 (3) 333-349 doi:10.1016/s0377-0273(03)00412-8
Mashima, H. (2009) Genesis of high-magnesium andesites and associated basalts from Saga–Futagoyama, northwest Kyushu, southwest Japan. Journal of Volcanology and Geothermal Research, 187 (1) 106-116 doi:10.1016/j.jvolgeores.2009.07.021
KAMEI, A (2004) High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, southwest Japan arc: evidence from clinopyroxene and whole rock compositions. Lithos, 75 (3) 359-371 doi:10.1016/j.lithos.2004.03.006
Ayalew, Dereje, Gibson, Sally A. (2009) Head-to-tail transition of the Afar mantle plume: Geochemical evidence from a Miocene bimodal basalt–rhyolite succession in the Ethiopian Large Igneous Province. Lithos, 112 (3) 461-476 doi:10.1016/j.lithos.2009.04.005
Sawyer, E.W. (2010) Migmatites formed by water-fluxed partial melting of a leucogranodiorite protolith: Microstructures in the residual rocks and source of the fluid. Lithos, 116 (3) 273-286 doi:10.1016/j.lithos.2009.07.003
Oikawa, Teruki, Mashima, Hidehisa, Tanase, Atsushi, Ninomiya, Atusi, Umeda, Koji (2006) K-Ar age of high magnesium andesite dikes at the Toki River in Gifu Prefecture, central Japan. The Journal of the Geological Society of Japan, 112 (10) 616-619 doi:10.5575/geosoc.112.616
Ishimoto, Hiroyuki, Shuto, Kenji, Goto, Yoshihiko (2006) Middle Miocene to Quaternary primary basalt and high magnesian andesite magmas of North Hokkaido, Japan: Source mantle characteristics and degrees of partial melting. The Island Arc, 15 (2). 251-268 doi:10.1111/j.1440-1738.2006.00525.x
Taniuchi, Hajime, Kuritani, Takeshi, Nakagawa, Mitsuhiro (2020) Generation of calc-alkaline andesite magma through crustal melting induced by emplacement of mantle-derived water-rich primary magma: Evidence from Rishiri Volcano, southern Kuril Arc. Lithos, 354. 105362 doi:10.1016/j.lithos.2019.105362
 
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