LOWER MANTLE PHASE-TRANSITIONS MAY GENERALLY HAVE NEGATIVE PRESSURE-TEMPERATURE SLOPES

[1] AKIMOTO S, 1969, J GEOPHYS RES, V74, P273

[2] TEMPERATURE DEPENDENCE OF PROPERTIES OF MAGNESIUM FERRITE [J]. JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1966, 49 (05) : 257 - &

[3] Bassett W.A., 1969, T AM CRYSTALLOGR ASS, V5, P93

[4] RUTILE-TYPE COMPOUNDS .4. SIO2, GEO2 AND A COMPARISON WITH OTHER RUTILE-TYPE STRUCTURES [J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL CRYSTALLOGRAPHY AND CRYSTAL CHEMISTRY, 1971, B 27 (NOV15): : 2133 - &

[5] BUKOWINSKI MST, 1977, HIGH PRESSURE RES AP, P367

[6] CARMICHAEL ISE, 1979, EOS T AM GEOPHYS UNI, V60, P964

[7] ENTHALPY OF FORMATION OF SOME LIME SILICATES BY HIGH-TEMPERATURE SOLUTION CALORIMETRY, WITH DISCUSSION OF HIGH-PRESSURE PHASE-EQUILIBRIA [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1978, 42 (04) : 367 - 375

[8] DAVIES PK, 1979, EOS T AM GEOPHYS UNI, V60, P964

[9] Hafner S., 1961, Z KRISTALLOGR, V115, P321, DOI 10.1524/zkri.1961.115.16.321

[10] HELGESON HC, 1978, AM J SCI, V278, P1

[1] AKIMOTO S, 1969, J GEOPHYS RES, V74, P273

[2] TEMPERATURE DEPENDENCE OF PROPERTIES OF MAGNESIUM FERRITE [J]. JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1966, 49 (05) : 257 - &

[3] Bassett W.A., 1969, T AM CRYSTALLOGR ASS, V5, P93

[4] RUTILE-TYPE COMPOUNDS .4. SIO2, GEO2 AND A COMPARISON WITH OTHER RUTILE-TYPE STRUCTURES [J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL CRYSTALLOGRAPHY AND CRYSTAL CHEMISTRY, 1971, B 27 (NOV15): : 2133 - &

[5] BUKOWINSKI MST, 1977, HIGH PRESSURE RES AP, P367

[6] CARMICHAEL ISE, 1979, EOS T AM GEOPHYS UNI, V60, P964

[7] ENTHALPY OF FORMATION OF SOME LIME SILICATES BY HIGH-TEMPERATURE SOLUTION CALORIMETRY, WITH DISCUSSION OF HIGH-PRESSURE PHASE-EQUILIBRIA [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1978, 42 (04) : 367 - 375

[8] DAVIES PK, 1979, EOS T AM GEOPHYS UNI, V60, P964

[9] Hafner S., 1961, Z KRISTALLOGR, V115, P321, DOI 10.1524/zkri.1961.115.16.321

[10] HELGESON HC, 1978, AM J SCI, V278, P1