Crystallography Open Database

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

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9003777 CIFFe2 Mg O4F d -3 m :28.3549; 8.3549; 8.3549
90; 90; 90
583.208Antao, 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 = 1150 K, P = 6 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003778 CIFFe2 Mg O4F d -3 m :28.34531; 8.34531; 8.34531
90; 90; 90
581.202Antao, 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 = 970 K, P = 6 GPa during cooling
American Mineralogist, 2005, 90, 1500-1505
9003779 CIFFe2 Mg O4F d -3 m :28.3363; 8.3363; 8.3363
90; 90; 90
579.322Antao, 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 = 860 K, P = 6 GPa during cooling
American Mineralogist, 2005, 90, 1500-1505
9003780 CIFFe2 Mg O4F d -3 m :28.32646; 8.32646; 8.32646
90; 90; 90
577.273Antao, 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 = 700 K, P = 6 GPa during cooling
American Mineralogist, 2005, 90, 1500-1505
9003781 CIFFe2 Mg O4F d -3 m :28.33637; 8.33637; 8.33637
90; 90; 90
579.337Antao, 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 = 675 K, P = 5 GPa during heating
American Mineralogist, 2005, 90, 1500-1505

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