The partially dehydrated structure of natural heulandite : An in situ high temperature single crystal X-ray diffraction study
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概要
- 論文の詳細を見る
- 日本鉱物科学会の論文
- 2008-04-01
著者
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Kudoh Yasuhiro
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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Kudoh Yasuhiro
Institute Of Mineralogy Petrology And Economic Geology Tohoku University
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Komatsu Kazuki
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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KURIBAYASHI Takahiro
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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KHOBAER T.
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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Khobaer T.
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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Kuribayashi Takahiro
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
関連論文
- 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
- Crystal structural features of hydrous forsterite : Effect of Fe on the M-site vacancies, possible hydrogen positions and variation of the unit cell dimensions
- Pressure dependence of u parameter in ringwoodite up to 7.9 GPa