about
Boron-doped diamond heater and its application to large-volume, high-pressure, and high-temperature experiments.High-pressure synthesis of the cubic perovskite BaRuO3 and evolution of ferromagnetism in ARuO3 (A = Ca, Sr, Ba) ruthenatesA nearly water-saturated mantle transition zone inferred from mineral viscosity.Single-crystal metastable high-temperature C2/c clinoenstatite quenched rapidly from high temperature and high pressure.Precise determination of elastic constants by high-resolution inelastic X-ray scattering.Complete agreement of the post-spinel transition with the 660-km seismic discontinuity.Olivine-wadsleyite transition in the system (Mg,Fe)2SiO4Critical Behavior of the Ferromagnetic PerovskiteBaRuO3Why and How to Write a High-Impact Review Paper: Lessons From Eight Years of Editorial Board Service to Reviews of GeophysicsNew constraints on upper mantle creep mechanism inferred from silicon grain-boundary diffusion ratesHigh silicon self-diffusion coefficient in dry forsteriteSilicon and magnesium diffusion in a single crystal of MgSiO3perovskitePhase boundary between perovskite and post-perovskite structures in MnGeO3 determined by in situ X-ray diffraction measurements using sintered diamond anvilsPressure generation and investigation of the post-perovskite transformation in MgGeO3 by squeezing the Kawai-cell equipped with sintered diamond anvilsPhase boundary between ilmenite and perovskite structures in MnGeO3 determined by in situ X-ray diffraction measurementsA large-volume high-pressure and high-temperature apparatus for in situ X-ray observation, ‘SPEED-Mk.II’Phase transition of zircon at high P-T conditionsThermal expansion of Mg2SiO4ringwoodite at high pressuresDetermination of the phase boundary between theB1andB2phases in NaCl byin situx-ray diffractionHydrous olivine unable to account for conductivity anomaly at the top of the asthenosphereElectrical conductivity of silicate perovskite at lower-mantle conditionsDry mantle transition zone inferred from the conductivity of wadsleyite and ringwooditeCore formation in planetesimals triggered by permeable flowSmall effect of water on upper-mantle rheology based on silicon self-diffusion coefficientsMelting experiments of mantle materials under lower mantle conditions with implications for magma ocean differentiationPhase Relations in the System MgSiO3 -Al2 O3 up to 2300 K at Lower Mantle PressuresGeneration of pressures over 40 GPa using Kawai-type multi-anvil press with tungsten carbide anvilsHigh-pressure research in earth science: Crust, mantle, and coreSilicate diffusion in alkali-carbonatite and hydrous melts at 16.5 and 24GPa: Implication for the melt transport by dissolution–precipitation in the transition zone and uppermost lower mantleHigh pressure generation using scaled-up Kawai-cellPressless split-sphere apparatus equipped with scaled-up Kawai-cell for mineralogical studies at 10-20 GPaSystematic study of hydrogen incorporation into Fe-free wadsleyitePerformance of semi-sintered ceramics as pressure-transmitting media up to 30 GPaHydrogen incorporation into forsterite in Mg2SiO4–K2Mg(CO3)2–H2O and Mg2SiO4–H2O–C at 7.5–14.0 GPaCrystal Structure of New Carbon–Nitride-Related Material C$_{2}$N$_{2}$(CH$_{2}$)P-V-T relations of MgSiO3perovskite determined by in situ X-ray diffraction using a large-volume high-pressure apparatusP-V-Trelations of wadsleyite determined by in situ X-ray diffraction in a large-volume high-pressure apparatusEquation of state of (Mg0.8,Fe0.2)2SiO4ringwoodite from synchrotron X-ray diffraction up to 20 GPa and 1700 KHardness of polycrystalline SiO2 coesiteIncrease of the oxygen vacancy component in bridgmanite with temperature
P50
Q34955735-45F34735-7BDE-412E-A2CD-9B5A6A3C99D4Q36734659-30741D90-55BF-4942-A157-F4199502DD69Q41773625-4F6D22B6-A1D1-407C-89C7-716C9B24BFD7Q44199044-7E4825A6-65C5-499F-8F2E-3302EF690748Q51865596-F19422EB-E99D-45ED-AE84-60F68DB083B2Q55451595-6B34D066-741D-4251-AFE2-EC0487A96ED7Q56680244-6C64D712-82CE-47F9-B6C3-8A329D52BB1FQ56898829-DEB9E31B-D226-4480-8FCF-59CBDD03ABAEQ57083881-3DC95FF4-3B1F-4467-8E1D-D3E3CE5F737AQ57865889-464FCE57-C1D5-4408-8E1F-676C7273FF91Q57866125-0706E0A0-94C4-432A-B3B8-0D629E2BA119Q57866195-03014699-6B7C-4510-8C67-0A095E2ECD12Q57872946-17792D8B-D39C-40CC-ABF9-5A5BD2F4AEF4Q57872955-2074BE88-7D15-4F0C-B749-E2E10B362F6DQ57872984-239C87CA-54F7-4A16-8E13-95CE05300332Q57872989-395E14D4-3993-4185-AD77-CBB656B5DA69Q57872993-6C648031-7D7B-4930-BB3F-782E2D358490Q57873003-AE9D5968-97DC-4589-BA88-8DC572E08C26Q57873007-E72112E2-D023-42E3-AC9C-91CC82CBCBA1Q59056914-D73DE7A7-79BB-40DD-8BD7-8A6F08EE09CEQ59066714-35F3DDCB-EC37-4310-BFFE-93D22129AC8BQ59071936-8471293A-F16D-4FC9-82C4-6841AB1D66F3Q59084070-9C286F88-4FDD-4083-850E-02936B22A0DAQ59085749-60965433-7691-4A90-8032-BE8BC00E093CQ60016719-729E83E3-0043-41A7-A9F0-0F92927AE2C0Q60101710-28E5E39A-2800-4C87-94CF-B5B11F0E5FDEQ60176183-8521A9C5-44BC-481C-ABE3-CD97E31BEDC1Q60722192-44A37B47-9941-4EEF-BCD5-BE56F9F55A72Q60722241-BFE19320-C8D0-4D49-82E3-2A896B981743Q60722283-1763274E-B4CA-42E0-B0CB-A1824E795459Q60722298-495D0929-0FD3-43B7-8621-5DAF25029CFFQ60722308-EDCB1D0B-2349-4D58-BB29-19EA7469800DQ60722319-347ED57B-151A-44C4-B1DD-1053DA27DDBEQ60722332-CDD611A9-C1EB-4D3A-BA1D-E1BC5D77ADD5Q63645797-80E57B17-6A7C-4C22-8538-31C06EA46F4EQ63645801-E941777E-3B28-4BD0-B9EA-6F1D46305335Q63645803-2C321B73-047B-4D1C-9DA4-A9A58D95272FQ63645807-53BBD226-C895-4054-8250-EFBA965D79B2Q63930408-6C57BD70-40F3-4FFE-AC62-FFD2A08F61DFQ63930409-D615B256-7D00-47B0-B618-86EE4BD419EC
P50
description
hulumtues
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Tomoo Katsura
@ast
Tomoo Katsura
@en
Tomoo Katsura
@es
Tomoo Katsura
@nl
Tomoo Katsura
@sl
type
label
Tomoo Katsura
@ast
Tomoo Katsura
@en
Tomoo Katsura
@es
Tomoo Katsura
@nl
Tomoo Katsura
@sl
prefLabel
Tomoo Katsura
@ast
Tomoo Katsura
@en
Tomoo Katsura
@es
Tomoo Katsura
@nl
Tomoo Katsura
@sl
P1053
A-7483-2010
P106
P1153
7102140379
P21
P31
P3829
P3835
tomoo-katsura
P496
0000-0001-7857-5101