Crystallography Open Database

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Searching journal of publication like 'American Mineralogist' volume of publication is 90

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9003792 CIFFe2 Mg O4F d -3 m :28.40123; 8.40123; 8.40123
90; 90; 90		592.964Antao, S. M.; Hassan, I.; Crichton, W. A.; Parise, J. B.
Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1045 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003793 CIFFe2 Mg O4F d -3 m :28.41012; 8.41012; 8.41012
90; 90; 90		594.849Antao, S. M.; Hassan, I.; Crichton, W. A.; Parise, J. B.
Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1090 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003794 CIFFe2 Mg O4F d -3 m :28.41455; 8.41455; 8.41455
90; 90; 90		595.789Antao, S. M.; Hassan, I.; Crichton, W. A.; Parise, J. B.
Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1110 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003795 CIFFe2 Mg O4F d -3 m :28.42331; 8.42331; 8.42331
90; 90; 90		597.652Antao, S. M.; Hassan, I.; Crichton, W. A.; Parise, J. B.
Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1220 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003796 CIFFe2 Mg O4F d -3 m :28.4344; 8.4344; 8.4344
90; 90; 90		600.016Antao, S. M.; Hassan, I.; Crichton, W. A.; Parise, J. B.
Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1310 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505

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