References
- Suzuki A, Ohtani E, Kamada T. A new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000°C. Phys Chem Minerals. 2000;27:689–693. doi: 10.1007/s002690000120
- Terasaki H, Ohtani E, Sakai T, et al. Stability of Fe-Ni hydride after the reaction between Fe-Ni alloy and hydrous phase (δ-AlOOH) up to 1.2 Mbar: possibility of H contribution to the core density deficit. Phys Earth Planet Inter. 2012;194-195:18–24. doi: 10.1016/j.pepi.2012.01.002
- Ohira I, Ohtani E, Sakai T, et al. Stability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantle. Earth Planet Sci Lett. 2014;401:12–17. doi: 10.1016/j.epsl.2014.05.059
- Sano-Furukawa A, Komatsu K, Vanpeteghem CB, et al. Neutron diffraction study of δ-AlOOD at high pressure and its implication for symmetrization of the hydrogen bond. Am Miner. 2008;93:1558–1567. doi: 10.2138/am.2008.2849
- Vanpeteghem CB, Ohtani E, Kondo T. Equation of state of the hydrous phase δ-AlOOH at room temperature up to 22.5 GPa. Geophys Res Lett. 2002;29:23. doi: 10.1029/2001GL014224
- Suzuki A. Compressibility of the high-pressure polymorph of AlOOH to 17 GPa. Mineral Mag. 2009;73:479–485. doi: 10.1180/minmag.2009.073.3.479
- Suzuki A. High-pressure X-ray diffraction study of ε-FeOOH. Phys Chem Minerals. 2010;37:153–157. doi: 10.1007/s00269-009-0319-x
- Suzuki A. Compression behavior of manganite. J Mineral Petrol Sci. 2013;108:295–299. doi: 10.2465/jmps.130621b
- Suzuki A. Pressure-volume-temperature equation of state of ε-FeOOH to 11 GPa and 700 K. J Mineral Petrol Sci. 2016;111:420–424. doi: 10.2465/jmps.160719c
- Sano-Furukawa A, Kagi H, Natai T, et al. Change in compressibility of δ-AlOOH and δ-AlOOD at high pressure: a study of isotope effect and hydrogen-bond symmetrization. Am Miner. 2009;94:1255–1261. doi: 10.2138/am.2009.3109
- Sano-Furukawa A, Yagi T, Okada T, et al. Compression behaviors of distorted rutile-type hydrous phases, MOOH (M = Ga, In, Cr) and CrOOD. Phys Chem Minerals. 2012;39:375–383. doi: 10.1007/s00269-012-0487-y
- Suzuki A, Ohtani E, Funakoshi K, et al. Viscosity of albite melt at high pressure and high temperature. Phys Chem Minerals. 2002;29:159–165. doi: 10.1007/s00269-001-0216-4
- Nishiyama N, Wang Y, Sanehira T, et al. Development of the multi-anvil assembly 6-6 for DIA and D-DIA type high pressure apparatus. High Press Res. 2008;28:307–314. doi: 10.1080/08957950802250607
- Seto Y, Nishio-Hamane D, Nagai T, et al. Development of a software suite on X-ray diffraction experiments. Rev High Pressure Sci Technol. 2010;20:269–276. Japanese. doi: 10.4131/jshpreview.20.269
- Brown JM. The NaCl pressure standard. J Appl Phys. 1999;86:5801–5808. doi: 10.1063/1.371596
- Angel RJ, Gonzalez-Platas J, Alvaro M, et al. Eosfit7c and a Fortran module (library) for equation of state calculations. Z Krist. 2014;229:405–419.
- Gleason AE, Jeanloz R, Kunz M. Pressure-temperature stability studies of FeOOH using X-ray diffraction. Am Miner. 2008;93:1882–1885. doi: 10.2138/am.2008.2942
- Wiethoff F, Grevel K-D, Marler B, et al. P-V-T behavior of FeO(OH) and MnO(OH). Phys Chem Minerals. 2017;44:567–576. doi: 10.1007/s00269-017-0884-3
- Sano A, Yagi T, Okada T, et al. X-ray diffraction study of high pressure transition in InOOH. J Mineral Petrol Sci. 2008;103:152–155. doi: 10.2465/jmps.071022m
- Nishi M, Kuwayama Y, Tsuchiya J, et al. The pyrite-type high-pressure form of FeOOH. Nature. 2017;547:205–208. doi: 10.1038/nature22823
- Shannon RD. Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Cryst. 1976;32:751–767. doi: 10.1107/S0567739476001551