HOW AND WHY DOES OLIVINE TRANSFORM TO SPINEL

被引:18
作者
GREEN, HW
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D O I
10.1029/GL011i009p00817
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
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页码:817 / 820
页数:4
相关论文
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[1]   OLIVINE TO SPINEL TRANSFORMATION IN MG2SIO4 VIA FAULTED STRUCTURES [J].
BOLAND, JN ;
LIU, LG .
NATURE, 1983, 303 (5914) :233-235
[2]   MECHANISM OF THE OLIVINE TO SPINEL PHASE-TRANSFORMATION IN NI2SIO4 [J].
BOLAND, JN ;
LIEBERMANN, RC .
GEOPHYSICAL RESEARCH LETTERS, 1983, 10 (01) :87-90
[3]  
BURNS RG, 1972, 24TH P INT GEOL C, V14, P113
[5]   CHARGE-TRANSFER AND O- FORMATION IN HIGH AND ULTRAHIGH PRESSURE PHASE-TRANSITIONS [J].
FREUND, F .
BULLETIN DE MINERALOGIE, 1981, 104 (2-3) :177-185
[6]   INVESTIGATION OF THE MECHANISM OF THE OLIVINE-SPINEL TRANSITION IN FAYALITE BY SYNCHROTRON RADIATION [J].
FURNISH, MD ;
BASSETT, WA .
JOURNAL OF GEOPHYSICAL RESEARCH, 1983, 88 (NB12) :333-341
[7]   METASTABLE GROWTH OF COESITE IN HIGHLY STRAINED QUARTZ [J].
GREEN, HW .
JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 17 (14) :2478-+
[8]  
GREEN HW, 1983, GEOPHYS MONOG
[9]   ON THE MECHANISM OF THE OLIVINE SPINEL PHASE-TRANSFORMATION [J].
HAMAYA, N ;
AKIMOTO, S .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1982, 29 (01) :6-11
[10]  
HAMAYA N, 1982, HIGH PRESSURE RES GE, P373