Raman study of phase D at various pressures and temperatures

被引:11
作者
Liu, LG [1 ]
Lin, CC
Irifune, T
Mernagh, TP
机构
[1] Acad Sinica, Inst Earth Sci, Taipei 115, Taiwan
[2] Ehime Univ, Dept Earth Sci, Matsuyama, Ehime 790, Japan
[3] Australian Geol Survey Org, Canberra, ACT 2601, Australia
关键词
D O I
10.1029/98GL01415
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Samples of phase D were synthesized in high pressure and high temperature experiments with a multi anvil press. Phase D may have a chemical range of Mg/Si = 0.65 +/- 0.05 and H(2)O in the range 6 similar to 14 wt% on the basis of electron microprobe analyses. The nature of phase D was characterized by both powder X-ray diffraction and Raman spectroscopy. The resolution of the Raman spectra of phase D is in general very poor, though the X-ray diffraction data suggest that it is well crystalline. No clear OH Raman band of phase D was demonstrated, however. Variations of Raman spectra of phase D were investigated up to 18 GPa at room temperature and in the range 81 - 373 K at atmospheric pressure. Lower temperatures and/or high hydrostatic pressures did not improve the quality of the spectra. Phase D is extremely unstable when it was irradiated by laser and/or heated above 373 K at atmospheric pressure. Among the silicate vibrations, the pressure variation has been studied for only two bands and the temperature variation for four bands. The Raman frequencies for these bands of phase D increase with increasing pressure but decrease with increasing temperature, which are the same as the other dense hydrous magnesium silicates so far studied.
引用
收藏
页码:3453 / 3456
页数:4
相关论文
共 24 条
[1]   EFFECT OF WATER ON MELTING PHASE-RELATIONS AND MELT COMPOSITION IN THE SYSTEM MG2SIO4-MGSIO3-H2O UP TO 15 GPA [J].
INOUE, T .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1994, 85 (3-4) :237-263
[2]   Amorphization of serpentine at high pressure and high temperature [J].
Irifune, T ;
Kuroda, K ;
Funamori, N ;
Uchida, T ;
Yagi, T ;
Inoue, T ;
Miyajima, N .
SCIENCE, 1996, 272 (5267) :1468-1470
[3]   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
[4]  
Kuroda K, 1998, GEOPH MONOG SERIES, V101, P545
[5]   PHASES AND ELECTRICAL-CONDUCTIVITY OF A HYDROUS SILICATE ASSEMBLAGE AT LOWER-MANTLE CONDITIONS [J].
LI, XY ;
JEANLOZ, R .
NATURE, 1991, 350 (6316) :332-334
[6]  
LIU L, 1998, IN PRESS GEOPHYS RES
[7]  
LIU L, 1994, HIGH TEMP HIGH PRESS, V26, P631
[8]  
LIU L, 1998, IN PRESS J PHYS CHEM
[9]   HIGH-PRESSURE RAMAN-SPECTRA OF BETA-MG2SIO4,GAMMA-MG2SIO4, MGSIO3-ILMENITE AND MGSIO3-PEROVSKITE [J].
LIU, LG ;
MERNAGH, TP ;
IRIFUNE, T .
JOURNAL OF PHYSICS AND CHEMISTRY OF SOLIDS, 1994, 55 (02) :185-193
[10]   Raman spectra of phase E at various pressures and temperatures with geophysical implications [J].
Liu, LG ;
Mernagh, TP ;
Lin, CC ;
Irifune, T .
EARTH AND PLANETARY SCIENCE LETTERS, 1997, 149 (1-4) :57-65