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Suzuki, A., Ohtani, E., Kamada, T. (2000) A new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000 °C. Physics and Chemistry of Minerals, 27 (10) 689-693 doi:10.1007/s002690000120

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Reference TypeJournal (article/letter/editorial)
TitleA new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000 °C
JournalPhysics and Chemistry of Minerals
AuthorsSuzuki, A.Author
Ohtani, E.Author
Kamada, T.Author
Year2000 (December 14)Volume27
Issue10
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s002690000120Search in ResearchGate
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Mindat Ref. ID152692Long-form Identifiermindat:1:5:152692:3
GUID0
Full ReferenceSuzuki, A., Ohtani, E., Kamada, T. (2000) A new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000 °C. Physics and Chemistry of Minerals, 27 (10) 689-693 doi:10.1007/s002690000120
Plain TextSuzuki, A., Ohtani, E., Kamada, T. (2000) A new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000 °C. Physics and Chemistry of Minerals, 27 (10) 689-693 doi:10.1007/s002690000120
In(2000, December) Physics and Chemistry of Minerals Vol. 27 (10) Springer Science and Business Media LLC

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Kudoh, Y., Nagase, T., Sasaki, S., Tanaka, M., Kanzaki, M. (1997) Phase F, a New Hydrous Magnesium Silicate Synthesized at 1000 °C and 17 GPa: Crystal Structure and Estimated Bulk Modulus. Physics and Chemistry of Minerals, 24 (8) 601 doi:10.1007/s002690050078
Kudoh, Y.; Nagase, T.; Sasaki, S.; Tanaka, M.; Kanzaki, M. (1995) Phase F, a new hydrous magnesium silicate synthesized at 1000 °C and 17 GPa: Crystal structure and estimated bulk modulus. Physics and Chemistry of Minerals, 22 (5). 295-299 doi:10.1007/bf00202769
Kudoh, Y., Kuribayashi, T., Suzuki, A., Ohtani, E., Kamada, T. (2004) Space group and hydrogen sites of ?-AlOOH and implications for a hypothetical high-pressure form of Mg(OH)2. Physics and Chemistry of Minerals, 31 (6) doi:10.1007/s00269-004-0404-0
Kudoh, Y., Nagase, T., Mizohata, H., Ohtani, E., Sasaki, S., Tanaka, M. (1997) Structure and crystal chemistry of Phase G, A new hydrous magnesium silicate synthesized at 22 GPa and 1050°C. Geophysical Research Letters, 24 (9) 1051-1054 doi:10.1029/97gl00875
Ohtani, E., Mizobata, H., Yurimoto, H. (2000) Stability of dense hydrous magnesium silicate phases in the systems Mg 2 SiO 4 -H 2 O and MgSiO 3 -H 2 O at pressures up to 27 GPa. Physics and Chemistry of Minerals, 27 (8) 533-544 doi:10.1007/s002690000097
Ohtani, Eiji, Litasov, Konstantin, Suzuki, Akio, Kondo, Tadashi (2001) Stability field of new hydrous phase, δ-AlOOH, with implications for water transport into the deep mantle. Geophysical Research Letters, 28 (20) 3991-3993 doi:10.1029/2001gl013397
Vanpeteghem, Carine B. (2002) Equation of state of the hydrous phase δ-AlOOH at room temperature up to 22.5 GPa. Geophysical Research Letters, 29 (7) doi:10.1029/2001gl014224
Bindi, L., Nishi, M., Tsuchiya, J., Irifune, T. (2014) Crystal chemistry of dense hydrous magnesium silicates: The structure of phase H, MgSiH2O4, synthesized at 45 GPa and 1000  C. American Mineralogist, 99 (8) 1802-1805 doi:10.2138/am.2014.4994
Not Available, Not Available (2001) Erratum: Phys Chem Minerals (2000) 27: 650-655 and Phys Chem Minerals (2000) 27: 689-693. Physics and Chemistry of Minerals, 28 (5) 364 doi:10.1007/s002690100172
Kudoh, Y., Kuribayashi, T., Mizobata, H., Ohtani, E. (2000) Structure and cation disorder of hydrous ringwoodite, γ-Mg 1.89 Si 0.98 H 0.30 O 4. Physics and Chemistry of Minerals, 27 (7) 474-479 doi:10.1007/s002690000091
A., , B.T., , V., , M., (2019) High‐Temperature Evolution of Point Defect Equilibria in Hydrous Forsterite Synthesized at 1100 °C and up to 4 GPa. Minerals, 9 (10) 574 doi:10.3390/min9100574
 
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