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.
Papers
More filters
Journal ArticleDOI
Across-arc variations of isotope and trace element compositions from Quaternary basaltic volcanic rocks in northeastern Japan: Implications for interaction between subducted oceanic slab and mantle wedge
Tomoyuki Shibata,Eizo Nakamura +1 more
TL;DR: Isotopic compositions of Pb, Sr, and Nd and concentrations of trace elements were determined for Quaternary island arc basaltic rocks from northeastern Japan.
Journal ArticleDOI
Boron isotope geochemistry of metasedimentary rocks and tourmalines in a subduction zone metamorphic suite
Toshio Nakano,Eizo Nakamura +1 more
TL;DR: In this paper, the behavior of boron and its isotope fractionation during subduction zone metamorphism were determined for metasedimentary rocks and tourmalines from the Sambagawa Metamorphic Belt, central Shikoku, Japan.
Journal ArticleDOI
Coupled Lu–Hf and Sm–Nd geochronology constrains garnet growth in ultra‐high‐pressure eclogites from the Dabie orogen
TL;DR: In this article, three eclogites, sampled from Zhujiachong, Huangzhen and Shima, yield Lu-Hf ages of 240.0, 224.4±1.9 and 230.5±5.1, respectively.
Journal ArticleDOI
The influence of subduction processes on the geochemistry of Japanese alkaline basalts
TL;DR: This paper showed that the geochemistry of alkali basalts from Japan and eastern Asia varies systematically with distance from the Japanese island-arc, and they suggested that the northeastern island arboricity of these basalts were derived from a normal upper mantle source altered by fluids or melts released from the underlying subducted Pacific plate.
Journal ArticleDOI
Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle
TL;DR: Li concentrations and isotopic compositions of coexisting minerals (ol, opx, and cpx) from peridotite xenoliths entrained in the Hannuoba Tertiary basalts, North China Craton, provide insight into Li isotopic fractionation between mantle minerals during melt-rock interaction in the considerably thinned lithospheric mantle as discussed by the authors.