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Stability of magnesite and its high-pressure form in the lowermost mantle

Nature, 2004-01, Vol.427 (6969), p.60-63

2004

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In situ X-ray observations of phase assemblages in peridotite and basalt compositions at lower mantle conditions: Implications for density of subducted oceanic plate

Journal of Geophysical Research - Solid Earth, 2005-02, Vol.110 (B2), p.B02208-n/a

2005

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Transmission electron microscope observation of the high-pressure form of magnesite retrieved from laser heated diamond anvil cell

Earth and planetary science letters, 2005-10, Vol.239 (1), p.98-105

2005

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Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

Nature (London), 1998-04, Vol.392 (6677), p.702-705

1998

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High pressure and high temperature phase transitions of FeO

Physics of the earth and planetary interiors, 2004-08, Vol.146 (1), p.273-282

2004

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Construction of laser-heated diamond anvil cell system for in situ x-ray diffraction study at SPring-8

Review of Scientific Instruments, 2001-02, Vol.72 (2), p.1289-1292

2001

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Crystal Structure Analysis of a Hexatungstate by a High-Energy X-ray Diffraction Experiment Using an Imaging Plate Weissenberg Camera at the BL04B2 Beamline of SPring-8

Chemistry letters, 2001-08, Vol.30 (8), p.804-805

2001

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A Study on the Characteristics of Output Vocabulary in Essays Written by Korean Native Japanese Learners and Native Japanese Speakers

The Journal of Humanities, 2023-11, Vol.57, p.239-274

2023

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Small angle X-ray scattering measurements for supercritical fluid metals using synchrotron radiation

Journal of non-crystalline solids, 2002-10, Vol.312, p.269-273

2002

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Post-stishovite phase boundary in SiO2 determined by in situ X-ray observations

Earth and planetary science letters, 2002, Vol.197 (3-4), p.187-192

2002

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The postspinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction

Science (American Association for the Advancement of Science), 1998-03, Vol.279 (5357), p.1698-1700

1998

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Phase transformations in serpentine and transportation of water into the lower mantle

Geophysical research letters, 1998-01, Vol.25 (2), p.203-206

1998

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In situ X-ray observations of phase assemblages in peridotite and basalt compositions at lower mantle conditions : Implications for density of subducted oceanic plate

Journal of geophysical research, 2005, Vol.110 (B2), p.B02208.1-B02208.11

2005

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日本語母語話者と韓国人日本語学習者による終助詞｢よ｣の使用実態‒談話完成テストの調査結果に基づいて

The Japanese Modern Association of Korea, 2019-05 (64), p.55-78

一色舞子

2019

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Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

Nature (London), 1998-04, Vol.392 (6678), p.702-705

1998

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Post-stishovite phase boundary in SiOd2 determined by in situ X-ray observations

Earth and planetary science letters, 2002-04, Vol.197 (3-4), p.187-192

2002

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Mg/Si ratios of aqueous fluids coexisting with forsterite and enstatite based on the phase relations in the Mg 2 SiO 4 -SiO 2 -H 2 O system

The American mineralogist, 2004-10, Vol.89 (10), p.1433-1437

2004

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Post-stishovite phase boundary in SiO 2 determined by in situ X-ray observations

Earth and planetary science letters, 2002, Vol.197 (3), p.187-192

2002

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Phase boundary between rutile-type and CaCl 2 -type germanium dioxide determined by in situ X-ray observations

The American mineralogist, 2002-01, Vol.87 (1), p.99-102

2002

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Structure of pressure-induced amorphous form of SnI 4 at high pressure

Physical review. B, Condensed matter and materials physics, 2009-08, Vol.80 (5), Article 054201

2009

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The postpinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction

Science (American Association for the Advancement of Science), 1998-03, Vol.270 (5357), p.1698

1998

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The Postspinel Phase Boundary in Mg$_2$SiO$_4$ Determined by in Situ X-ray Diffraction

Science (American Association for the Advancement of Science), 1998-03, Vol.279 (5357), p.1698-1700

1998

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Stability of magnesite and its high-pressure form in the lowermost mantle

In situ X-ray observations of phase assemblages in peridotite and basalt compositions at lower mantle conditions: Implications for density of subducted oceanic plate

Transmission electron microscope observation of the high-pressure form of magnesite retrieved from laser heated diamond anvil cell

Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

High pressure and high temperature phase transitions of FeO

Construction of laser-heated diamond anvil cell system for in situ x-ray diffraction study at SPring-8

Crystal Structure Analysis of a Hexatungstate by a High-Energy X-ray Diffraction Experiment Using an Imaging Plate Weissenberg Camera at the BL04B2 Beamline of SPring-8

A Study on the Characteristics of Output Vocabulary in Essays Written by Korean Native Japanese Learners and Native Japanese Speakers

Small angle X-ray scattering measurements for supercritical fluid metals using synchrotron radiation

Post-stishovite phase boundary in SiO2 determined by in situ X-ray observations

The postspinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction

Phase transformations in serpentine and transportation of water into the lower mantle

In situ X-ray observations of phase assemblages in peridotite and basalt compositions at lower mantle conditions : Implications for density of subducted oceanic plate

日本語母語話者と韓国人日本語学習者による終助詞｢よ｣の使用実態‒談話完成テストの調査結果に基づいて

Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

Post-stishovite phase boundary in SiOd2 determined by in situ X-ray observations

Mg/Si ratios of aqueous fluids coexisting with forsterite and enstatite based on the phase relations in the Mg 2 SiO 4 -SiO 2 -H 2 O system

Post-stishovite phase boundary in SiO 2 determined by in situ X-ray observations

Phase boundary between rutile-type and CaCl 2 -type germanium dioxide determined by in situ X-ray observations

Structure of pressure-induced amorphous form of SnI 4 at high pressure

The postpinel phase boundary in Mg2SiO4 determined by in situ X-ray diffraction

The Postspinel Phase Boundary in Mg$_2$SiO$_4$ Determined by in Situ X-ray Diffraction

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