Crystallography Open Database
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Result: there are 316 entries in the selection
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Searching journal of publication like 'American Mineralogist' volume of publication is 90
COD ID ![]() |
Links | Formula ![]() |
Space group ![]() |
Cell parameters | Cell volume ![]() |
Bibliography |
|---|---|---|---|---|---|---|
| 9003802 | CIF | Fe2 Mg O4 | F d -3 m :2 | 8.41033; 8.41033; 8.41033 90; 90; 90 | 594.893 | Antao, 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 = 1030 K, P = 3 GPa during cooling American Mineralogist, 2005, 90, 1500-1505 |
| 9003803 | CIF | Fe2 Mg O4 | F d -3 m :2 | 8.39887; 8.39887; 8.39887 90; 90; 90 | 592.465 | Antao, 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 = 890 K, P = 3 GPa during cooling American Mineralogist, 2005, 90, 1500-1505 |
| 9003804 | CIF | Fe2 Mg O4 | F d -3 m :2 | 8.38636; 8.38636; 8.38636 90; 90; 90 | 589.821 | Antao, 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 = 560 K, P = 3 GPa during cooling American Mineralogist, 2005, 90, 1500-1505 |
| 9003805 | CIF | F3 Mg Na | P b n m | 5.2768; 5.4213; 7.5548 90; 90; 90 | 216.121 | Chen, J.; Liu, H.; Martin, C. D.; Parise, J. B.; Weidner, D. J. Crystal chemistry of NaMgF3 perovskite and high pressure and temperature Sample: P = 4 GPa, T = 25 C American Mineralogist, 2005, 90, 1534-1539 |
| 9003806 | CIF | F3 Mg Na | P b n m | 5.3047; 5.4282; 7.5864 90; 90; 90 | 218.45 | Chen, J.; Liu, H.; Martin, C. D.; Parise, J. B.; Weidner, D. J. Crystal chemistry of NaMgF3 perovskite and high pressure and temperature Sample: P = 4 GPa, T = 200 C American Mineralogist, 2005, 90, 1534-1539 |
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