RETRACTED: PHASE-F, A NEW HYDROUS MAGNESIUM-SILICATE SYNTHESIZED AT 1000-DEGREES-C AND 17 GPA - CRYSTAL-STRUCTURE AND ESTIMATED BULK MODULUS (RETRACTED ARTICLE. SEE VOL 24, PG 601, 1997)

被引:19
作者
KUDOH, Y
NAGASE, T
SASAKI, S
TANAKA, M
机构
[1] TOKYO INST TECHNOL, ENGN MAT RES LAB, YOKOHAMA, KANAGAWA 227, JAPAN
[2] NATL LAB HIGH ENERGY PHYS, PHOTON FACTORY, TSUKUBA, IBARAKI 305, JAPAN
[3] TOKYO INST TECHNOL, DEPT INORGAN MAT, TOKYO 152, JAPAN
关键词
D O I
10.1007/BF00202769
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The structure of phase F, a non-stoichiometric hydrous silicate synthesized in a uniaxial, split-sphere, multi-anvil apparatus at conditions of 17 GPa and 1000 degrees C, has been solved and refined in space group P6(3)cm, using synchrotron X-ray data for a single crystal of a size 18 x 24 x 30 mu m. The composition and unit cell for phase F are Mg3.35Si5.51H7.26O18, a = 5.073(3) Angstrom c = 14.013(9) Angstrom, V = 312.3(5) Angstrom(3). The structure contains layers with many similarities to superhydrous phase B. The layers of oxygen atoms are stacked in the ABCBAC-type double cubic closest packing arrangement. The bulk modulus of phase F was estimated from the structural and compositional relationship to superhydrous phase B and periclase.
引用
收藏
页码:295 / 299
页数:5
相关论文
共 16 条
[1]  
[Anonymous], 1974, INT TABLES XRAY CRYS
[2]  
BASS JD, 1991, T AM GEOPHYS UNION, V72, P499
[3]  
FAIRBAIRN HW, 1943, GEOL SOC AM BULL, V54, P1305
[4]  
FINGER LW, 1991, AM MINERAL, V76, P1
[5]   PHASE-RELATIONS IN THE TRANSITION ZONE [J].
GASPARIK, T .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B10) :15751-15769
[6]  
HAZEN RM, 1990, PHYS CHEM MINER, V17, P416
[7]  
HORIUCHI H, 1979, AM MINERAL, V64, P593
[8]   STABILITY OF HYDROUS MAGNESIUM SILICATES IN THE MANTLE TRANSITION ZONE [J].
KANZAKI, M .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1991, 66 (3-4) :307-312
[9]  
Kanzaki M, 1989, EOS, V70, P508
[10]  
KUDOH Y, 1993, PHYS CHEM MINER, V19, P357