FROM THE SIMPLEST CHEMICAL-SYSTEM TO THE NATURAL ONE - GARNET PERIODOTITE BAROMETRY

[1] THE MUTUAL SOLUBILITY OF COEXISTING ORTHO-PYROXENE AND CLINOPYROXENE - TOWARD AN ABSOLUTE GEOTHERMOMETER FOR THE NATURAL SYSTEM [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1985, 76 (1-2) : 109 - 122

[2] PRESSURE AND TEMPERATURE-DEPENDENCE OF ELASTIC-CONSTANTS OF PYROPE GARNET [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (17): : 2529 - 2534

[3] BOYD FR, 1973, GEOCHIM COSMOCHIM AC, V37, P2533, DOI 10.1016/0016-7037(73)90263-9

[4] BOYD FR, 1974, CARNEGIE I WASH YB, V73, P285

[5] Boyd FR, 1970, MINERAL SOC AM SPEC, V3, P63

[6] ENTHALPIES OF FORMATION AT 970 K OF COMPOUNDS IN SYSTEM MGO-AL2O3-SIO2 FROM HIGH-TEMPERATURE SOLUTION CALORIMETRY [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1975, 39 (11) : 1487 - 1497

[7] REACTION ENSTATITESS + SILLIMANITE REVERSIBLE SAPPHIRINESS + QUARTZ IN SYSTEM MGO-AL2O3-SIO2 [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1972, 36 (01) : 49 - +

[8] DANCHIN RV, 1976, CARNEGIE I WASHINGTO, V75, P531

[9] EXPERIMENTAL-DETERMINATION OF SPINEL PERIDOTITE TO GARNET PERIDOTITE REACTION IN SYSTEM MGO-AL2O3-SIO2 IN RANGE 900-DEGREES TO 1100-DEGREES-C AND AL2O3 ISOPLETHS OF ENSTATITE IN SPINEL FIELD [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1978, 66 (02) : 189 - 201

[10] EVIDENCE FOR STRUCTURAL-CHANGES IN GARNET CAUSED BY CALCIUM SUBSTITUTION [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1980, 71 (03) : 281 - 282

[1] THE MUTUAL SOLUBILITY OF COEXISTING ORTHO-PYROXENE AND CLINOPYROXENE - TOWARD AN ABSOLUTE GEOTHERMOMETER FOR THE NATURAL SYSTEM [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1985, 76 (1-2) : 109 - 122

[2] PRESSURE AND TEMPERATURE-DEPENDENCE OF ELASTIC-CONSTANTS OF PYROPE GARNET [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (17): : 2529 - 2534

[3] BOYD FR, 1973, GEOCHIM COSMOCHIM AC, V37, P2533, DOI 10.1016/0016-7037(73)90263-9

[4] BOYD FR, 1974, CARNEGIE I WASH YB, V73, P285

[5] Boyd FR, 1970, MINERAL SOC AM SPEC, V3, P63

[6] ENTHALPIES OF FORMATION AT 970 K OF COMPOUNDS IN SYSTEM MGO-AL2O3-SIO2 FROM HIGH-TEMPERATURE SOLUTION CALORIMETRY [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1975, 39 (11) : 1487 - 1497

[7] REACTION ENSTATITESS + SILLIMANITE REVERSIBLE SAPPHIRINESS + QUARTZ IN SYSTEM MGO-AL2O3-SIO2 [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1972, 36 (01) : 49 - +

[8] DANCHIN RV, 1976, CARNEGIE I WASHINGTO, V75, P531

[9] EXPERIMENTAL-DETERMINATION OF SPINEL PERIDOTITE TO GARNET PERIDOTITE REACTION IN SYSTEM MGO-AL2O3-SIO2 IN RANGE 900-DEGREES TO 1100-DEGREES-C AND AL2O3 ISOPLETHS OF ENSTATITE IN SPINEL FIELD [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1978, 66 (02) : 189 - 201

[10] EVIDENCE FOR STRUCTURAL-CHANGES IN GARNET CAUSED BY CALCIUM SUBSTITUTION [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1980, 71 (03) : 281 - 282