Premium
Structure and crystal chemistry of Phase G, A new hydrous magnesium silicate synthesized at 22 GPa and 1050°C
Author(s) -
Kudoh Y.,
Nagase T.,
Mizohata H.,
Ohtani E.,
Sasaki S.,
Tanaka M.
Publication year - 1997
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/97gl00875
Subject(s) - stishovite , silicate , crystal structure , crystallography , magnesium , monochromator , crystal (programming language) , crystal chemistry , phase (matter) , chemistry , materials science , analytical chemistry (journal) , mineralogy , metallurgy , quartz , optoelectronics , wavelength , organic chemistry , chromatography , computer science , programming language
A single crystal of phase G, Mg 1.24 Si 1.76 H 2.48 O 6 synthesized at conditions of 1050°C and 22 GPa, using a multi‐anvil apparatus was studied at the Photon Factory BL‐10A beamline at the National Laboratory for High Energy Physics, Tukuba, Japan. With a (111) Si double‐crystal monochromator and a single crystal measuring 47 × 35 × 12 µm, intensities of 95 independent reflections were collected with sin θ/λ <0.72 Å −1 and Io >1.5 σ Io at a wave length of 0.6990 Å. The unit cell parameters obtained through the refinement of 23 reflections are: Trigonal, a=4.790 (3) Å, c=4.344 (3) Å, V=86.3 (2) ų. The result of structure analysis in space group P1m (No. 162) indicates that the structure of phase G has close structural similarity to that of stishovite,SiO 2 . The calculated density of phase G is 3.43 g/cm³, which is larger than any other known dense hydrous magnesium silicate, suggesting that phase G might be stable even under lower mantle conditions.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom