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takehiko hiraga
takehiko hiraga
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Year
Melt segregation and strain partitioning: Implications for seismic anisotropy and mantle flow
BK Holtzman, DL Kohlstedt, ME Zimmerman, F Heidelbach, T Hiraga, ...
Science 301 (5637), 1227-1230, 2003
5432003
Effect of water and stress on the lattice-preferred orientation of olivine
H Jung, I Katayama, Z Jiang, T Hiraga, SI Karato
Tectonophysics 421 (1-2), 1-22, 2006
4082006
Influence of melt on the creep behavior of olivine–basalt aggregates under hydrous conditions
S Mei, W Bai, T Hiraga, DL Kohlstedt
Earth and Planetary Science Letters 201 (3-4), 491-507, 2002
2472002
Grain boundaries as reservoirs of incompatible elements in the Earth's mantle
T Hiraga, IM Anderson, DL Kohlstedt
Nature 427 (6976), 699-703, 2004
1872004
Olivine crystals align during diffusion creep of Earth’s upper mantle
T Miyazaki, K Sueyoshi, T Hiraga
Nature 502 (7471), 321-326, 2013
1482013
Experimental study of attenuation and dispersion over a broad frequency range: 2. The universal scaling of polycrystalline materials
C McCarthy, Y Takei, T Hiraga
Journal of Geophysical Research: Solid Earth 116 (B9), 2011
1102011
Water weakening of clinopyroxene in the dislocation creep regime
S Chen, T Hiraga, DL Kohlstedt
Journal of Geophysical Research: Solid Earth 111 (B8), 2006
1082006
Grain growth systematics for forsteriteħenstatite aggregates: Effect of lithology on grain size in the upper mantle
T Hiraga, C Tachibana, N Ohashi, S Sano
Earth and Planetary Science Letters 291 (1-4), 10-20, 2010
1072010
Mantle superplasticity and its self-made demise
T Hiraga, T Miyazaki, M Tasaka, H Yoshida
Nature 468 (7327), 1091-1094, 2010
932010
Chemistry of grain boundaries in mantle rocks
T Hiraga, IM Anderson, DL Kohlstedt
American Mineralogist 88 (7), 1015-1019, 2003
802003
Effect of H+ on Fe–Mg interdiffusion in olivine,(Fe, Mg) 2SiO4
Z Wang, T Hiraga, DL Kohlstedt
Applied physics letters 85 (2), 209-211, 2004
782004
Synthesis of highly dense and fine-grained aggregates of mantle composites by vacuum sintering of nano-sized mineral powders
S Koizumi, T Hiraga, C Tachibana, M Tasaka, T Miyazaki, T Kobayashi, ...
Physics and Chemistry of Minerals 37, 505-518, 2010
632010
Influence of mineral fraction on the rheological properties of forsterite+ enstatite during grain‐size‐sensitive creep: 2. Deformation experiments
M Tasaka, T Hiraga, ME Zimmerman
Journal of Geophysical Research: Solid Earth 118 (8), 3991-4012, 2013
592013
Influence of mineral fraction on the rheological properties of forsterite+ enstatite during grain‐size‐sensitive creep: 1. Grain size and grain growth laws
M Tasaka, T Hiraga
Journal of Geophysical Research: Solid Earth 118 (8), 3970-3990, 2013
542013
Equilibrium interface segregation in the diopside–forsterite system I: Analytical techniques, thermodynamics, and segregation characteristics
T Hiraga, DL Kohlstedt
Geochimica et Cosmochimica Acta 71 (5), 1266-1280, 2007
522007
Structure and chemistry of grain boundaries in deformed, olivine+ basalt and partially molten lherzolite aggregates: evidence of melt-free grain boundaries
T Hiraga, I Anderson, M Zimmerman, S Mei, D Kohlstedt
Contributions to Mineralogy and Petrology 144, 163-175, 2002
522002
Equilibrium interface segregation in the diopside–forsterite system II: applications of interface enrichment to mantle geochemistry
T Hiraga, MM Hirschmann, DL Kohlstedt
Geochimica et Cosmochimica Acta 71 (5), 1281-1289, 2007
512007
Interfacial energies for quartz and albite in pelitic schist
T Hiraga, O Nishikawa, T Nagase, M Akizuki, DL Kohlstedt
Contributions to Mineralogy and Petrology 143 (6), 664-672, 2002
442002
Grain‐to multiple‐grain‐scale deformation processes during diffusion creep of forsterite+ diopside aggregate: 1. Direct observations
G Maruyama, T Hiraga
Journal of Geophysical Research: Solid Earth 122 (8), 5890-5915, 2017
432017
Morphology of intergranular pores and wetting angles in pelitic schists studied by transmission electron microscopy
T Hiraga, O Nishikawa, T Nagase, M Akizuki
Contributions to Mineralogy and Petrology 141, 613-622, 2001
432001
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