Crystallography Open Database

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

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9003772 CIFAl0.38 Be1.06 Ca1.71 Fe5.61 Mg0.12 Na0.29 O20 Si4.56 Sn0.03 Ti0.24P -110.322; 10.729; 8.8624
105.802; 96.185; 124.758
731.673Grew, E. S.; Barbier, J.; Britten, J.; Yates, M. G.; Polyakov, V. O.; Shcherbakova, E. P.; Halenius, U.; Shearer, C. K.
Makarochkinite, Ca2Fe2+4Fe3+TiSi4BeAlO20, a new beryllosilicate member of the aenigmatite-sapphirine-surinamite group from the Il'men Mountains (southern Urals), Russia Sample: N86
American Mineralogist, 2005, 90, 1402-1412
9003773 CIFFe2 Mg O4F d -3 m :28.32016; 8.32016; 8.32016
90; 90; 90
575.964Antao, 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 = 640 K, P = 6 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003774 CIFFe2 Mg O4F d -3 m :28.32711; 8.32711; 8.32711
90; 90; 90
577.408Antao, 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 = 740 K, P = 6 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003775 CIFFe2 Mg O4F d -3 m :28.33588; 8.33588; 8.33588
90; 90; 90
579.234Antao, 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 = 885 K, P = 6 GPa during heating
American Mineralogist, 2005, 90, 1500-1505
9003776 CIFFe2 Mg O4F d -3 m :28.34613; 8.34613; 8.34613
90; 90; 90
581.374Antao, 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 = 1020 K, P = 6 GPa during heating
American Mineralogist, 2005, 90, 1500-1505

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