Crystallography Open Database

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

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9003787 CIFFe2 Mg O4F d -3 m :28.35489; 8.35489; 8.35489
90; 90; 90		583.206Antao, 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 = 870 K, P = 5 GPa during cooling
American Mineralogist, 2005, 90, 1500-1505
9003788 CIFFe2 Mg O4F d -3 m :28.33319; 8.33319; 8.33319
90; 90; 90		578.674Antao, 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 = 620 K, P = 5 GPa during cooling
American Mineralogist, 2005, 90, 1500-1505
9003789 CIFFe2 Mg O4F d -3 m :28.36741; 8.36741; 8.36741
90; 90; 90		585.832Antao, 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 = 730 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003790 CIFFe2 Mg O4F d -3 m :28.37647; 8.37647; 8.37647
90; 90; 90		587.737Antao, 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 = 815 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003791 CIFFe2 Mg O4F d -3 m :28.38915; 8.38915; 8.38915
90; 90; 90		590.41Antao, 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 = 960 K, P = 3 GPa during heating
American Mineralogist, 2005, 90, 1500-1505

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