E
Eizo Nakamura
Researcher at Okayama University
Publications - 230
Citations - 9467
Eizo Nakamura is an academic researcher from Okayama University. The author has contributed to research in topics: Basalt & Metamorphism. The author has an hindex of 54, co-authored 218 publications receiving 8465 citations. Previous affiliations of Eizo Nakamura include University of Toronto & Geological Survey of Pakistan.
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Lithospheric-folding-based understanding on the origin of the back-arc basaltic magmatism beneath Jeju volcanic island
TL;DR: In this article, the authors investigate the subsurface structure of Jeju (Cheju) volcanic island and its vicinity, and propose an alternative hypothesis that the basaltic magma beneath the island could be caused by (episodic) lithospheric folding.
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Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif
Lalindra V. Ranaweera,Lalindra V. Ranaweera,Tsutomu Ota,Takuya Moriguti,Ryoji Tanaka,Eizo Nakamura +5 more
TL;DR: It is demonstrated that peridotites from the Horoman massif preserve the chemical signatures of sub-seafloor hydrothermal alteration at a mid-ocean ridge approximately one billion years ago, indicating that ancient SSH alteration resulting in the production of sulfide leads to Pb enrichment that could affect the present-day Pb isotopic evolution of the silicate earth.
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Silicate–SiO reaction in a protoplanetary disk recorded by oxygen isotopes in chondrules
Ryoji Tanaka,Eizo Nakamura +1 more
TL;DR: In this article, it was shown that for chondrules in unequilibrated enstatite chondrites, high-precision Δ17O values vary significantly and fall on an array with a steep slope of 127 on a threeoxygen-isotope plot.
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Gravity-induced diffusion of isotope atoms in monoatomic solid Se
Tsutomu Mashimo,Tsutomu Mashimo,Masao Ono,Xinsheng Huang,Yusuke Iguchi,Satoru Okayasu,Katsura Kobayashi,Eizo Nakamura +7 more
TL;DR: In this paper, a strong gravitational field resulted in the gravity-induced diffusion (sedimentation) of isotope atoms in monoatomic solid Se The layer crystalline morphology consisting of three zones of the fine-grained crystals, the long crystals and feather-shaped crystals grown parallel to gravity direction appeared in the specimen ultracentrifuged at (08 1)×106 G and at 190 °C Change in the concentration ratio 82Se/76Se of >08% was observed in the grown crystalline region.
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A new concept for the genesis of felsic magma: the separation of slab-derived supercritical liquid.
Hajime Taniuchi,Takeshi Kuritani,Takeshi Kuritani,Tetsuya Yokoyama,Tetsuya Yokoyama,Eizo Nakamura,Mitsuhiro Nakagawa +6 more
TL;DR: It is inferred that slab-derived supercritical liquid is an efficient transport medium for moving silicate-rich components from subducting slabs to the Earth’s surface, and that this process may have contributed to the growth of the continental crust.