Melting Relations of an Anhydrous Abyssal Basalt at High Pressures
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[1] E. Watson,et al. Adcumulus dunite growth in a laboratory thermal gradient , 1988 .
[2] O. Shimomura,et al. In situ observation of the olivine‐spinel phase transformation in Fe2SiO4 using synchrotron radiation , 1987 .
[3] E. Takahashi. Melting of a dry peridotite KLB‐1 up to 14 GPa: Implications on the Origin of peridotitic upper mantle , 1986 .
[4] Takumi Kato,et al. Stability of phase B, A hydrous magnesium silicate, to 2300°C at 20 GPA , 1985 .
[5] A. E. Ringwood,et al. Phase Transformations and Differentiation in Subducted Lithosphere: Implications for Mantle Dynamics, Basalt Petrogenesis, and Crustal Evolution , 1982, The Journal of Geology.
[6] H. Massonne,et al. The low‐high quartz and quartz‐coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO2 component on the low quartz‐coesite transition , 1980 .
[7] I. Kushiro. Changes in viscosity and structure of melt of NaAlSi2O6 composition at high pressures , 1976 .
[8] Keisuke Ito,et al. Melting and phase relations in an anhydrous basalt to 40 kilobars , 1967 .
[9] A. E. Ringwood,et al. The genesis of basaltic magmas , 1967 .
[10] D. Walker,et al. Abyssal tholeiites from the Oceanographer Fracture Zone , 1979 .