KY
Member Since 2014
Kosuke Yabe
Post-doctoral researcher, The University of Tokyo, Japan
Professional Experience
The University of Tokyo, Japan
Post-doctoral researcher
2023 - Present
Education
Earthquake Research Institute, The University of Tokyo
Doctorate
2020
Masters
2015
Honors & Awards
Mineral and Rock Physics Graduate Research Award
Received December 2021
Publications
Diffusion Creep Characteristics of Anorthite Revealed by Uni...
February 24, 2023
Grain‐Boundary Diffusion Creep of Olivine: 2. Solidus Effect...
August 26, 2020
Grain‐Boundary Diffusion Creep of Olivine: 1. Experiments at...
August 26, 2020
AGU Abstracts
Olivine Crystallographic Preferred Orientation (CPO) in Diffusion Creep and its Comparison to Mantle Peridotites
SEISMIC ANISOTROPY AND MANTLE DYNAMICS: OBSERVATIONS, MODELS, AND EXPERIMENTS III POSTER
study of earth's deep interior | 14 december 2023
NAHYEON KIM, Akihiro Ando, Kosuke Yabe, Takehiko H...
Olivine crystallographic preferred orientation (CPO) is a significant factor contributing to seismic anisotropy in the upper mantle. Recent studies in...
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Grain boundary chemistry and creep properties of olivine
FROM A SINGLE CRYSTAL ON UP: IN HONOR OF DAVID KOHLSTEDT'S CAREER II POSTER
mineral and rock physics | 13 december 2023
Takehiko Hiraga, NAHYEON KIM, Kosuke Yabe, Atsuro ...
Equilibrium Ca and Al grain boundary segregation has been known in olivine [1]. We synthesized fine-grained Fe-free and Fe-bearing olivine aggregates ...
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Grain growth-induced fabric transition
FROM GRAIN TO EARTH: UNDERSTANDING PLATE TECTONICS THROUGH ROCK MICROPHYSICS AND RECRYSTALLIZATION TO MANTLE-SCALE ANALYSES I ORAL
mineral and rock physics | 12 december 2023
Takehiko Hiraga, NAHYEON KIM, Kosuke Yabe
Many studies assume that olivine CPO results from dislocation processes; however, we have emphasized that CPO develops during diffusion creep dependin...
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