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Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University | 論文
- X-ray diffraction study of high pressure transition in InOOH
- Pressure dependence of u parameter in ringwoodite up to 7.9GPa
- High-pressure single crystal X-ray diffraction and FT-IR observation of natural chondrodite and synthetic OH-chondrodite
- Cation vacancies and possible hydrogen atom positions in Fe-bearing hydrous forsterite, Mg_Fe_Si_H_O_4, synthesized at 13.5GPa and 1400℃
- Cation vacancy and possible hydrogen positions in hydrous forsterite, Mg_Si_H_O_4, synthesized at 13.5GPa and 1300℃
- Orientational ordering of three SiO_4 tetrahedra in α'_L-Ca_Sr_SiO_4 that satisfies bond-valence requirements and avoids O-O repulsion
- The partially dehydrated structure of natural heulandite : An in situ high temperature single crystal X-ray diffraction study
- Compressibility of phase A, Mg_7Si_2H_6O_ up to 11.2 GPa
- Effect of temperature and pressure on the crystal structure of topaz, Al_2Sio_4(OH,F)_2
- Stability of dense hydrous magnesium silicate phase G in the transition zone and the lower mantle
- Raman spectroscopic study of a garnetite xenolith from Malaita, Southwest Pacific
- Application of FIB system to ultra-high-pressure Earth science
- 西オーストラリア・ハマースレイ地域の縞状鉄鉱床中に胚胎する高品位鉄鉱床の下盤頁岩の熱水変質について--全岩化学組成,同位体組成,流体包有物による検討
- A sample manuscript for Journal of Mineralogical and Petrological Sciences
- Possible Sites for Hydrogen in a New Hydrous Magnesium Silicate Phase G Synthesized at 22 GPa and 1050°C
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