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Katsura Kobayashi

Researcher at Okayama University

Publications -  85
Citations -  2437

Katsura Kobayashi is an academic researcher from Okayama University. The author has contributed to research in topics: Basalt & Eclogite. The author has an hindex of 29, co-authored 78 publications receiving 2089 citations.

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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.
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Fate of the subducted Farallon plate inferred from eclogite xenoliths in the Colorado Plateau

TL;DR: In this paper, the high-pressure mineral coesite in lawsonite-bearing eclogite xenoliths from the Colorado Plateau, United States has been found.

Fate of the subducted Farallon plate inferred from eclogite xenoliths in the Colorado Plateau

TL;DR: In this article, the high-pressure mineral coesite in lawsonite-bearing eclogite xenoliths from the Colorado Plateau, United States has been found.
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Space environment of an asteroid preserved on micrograins returned by the Hayabusa spacecraft

TL;DR: Impact appears to be an important process shaping the exteriors of not only large planetary bodies, such as the moon, but also low-gravity bodies such as asteroids, demonstrating the central role played by impact processes in the long-term evolution of planetary bodies.
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Lithium, boron, and lead isotope systematics of glass inclusions in olivines from Hawaiian lavas: evidence for recycled components in the Hawaiian plume

TL;DR: In this article, a set of synthetic glass standards with matrices similar to those of the target glass inclusions was prepared, and their isotopic variations were determined by TIMS.