Crystallography Open Database
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Displaying all data in COD
COD ID ![]() |
Links | Formula ![]() |
Space group ![]() |
Cell parameters | Cell volume ![]() |
Bibliography |
|---|---|---|---|---|---|---|
| 9015453 | CIF | Ca2.92 Ce0.54 F2.76 Gd0.04 La0.24 Na2.9 Nb0.75 Nd0.18 O15.24 Pr0.06 Si4 Sm0.04 Sr0.04 Ta0.01 Ti0.24 Y0.04 | P 1 21/c 1 | 7.468; 5.689; 18.891 90; 101.37; 90 | 786.841 | Sokolova, E.; Hawthorne, F. C. From structure topology to chemical composition. V. Titanium silicates: The crystal chemistry of nacareniobsite-(Ce) The Canadian Mineralogist, 2008, 46, 1333-1342 |
| 9015454 | CIF | Al2 Mg3 O12 Si3 | I a -3 d | 11.496; 11.496; 11.496 90; 90; 90 | 1519.29 | Nakatsuka, A.; Shimokawa, M.; Nakayama, N.; Ohtaka, O.; Arima, H.; Okube, M.; Yoshiasa, A. Static disorders of atoms and experimental determination of Debye temperature in pyrope: Low- and high-temperature single-crystal X-ray diffraction study Note: T = 672.9 K American Mineralogist, 2011, 96, 1593-1605 |
| 9015455 | CIF | Ca0.105 Fe0.075 H4 K0.025 Mg0.035 Mn0.165 Na1.645 Nb0.255 O11 Si2 Ti1.605 Zr0.005 | P -1 | 5.3875; 7.0579; 12.176 93.511; 107.943; 90.093 | 439.538 | Camara, F.; Sokolova, E.; Hawthorne, F. C.; Abdu, Y. From structure topology to chemical composition. IX. Titanium silicates: revision of the crystal chemistry of lomonosovite and murmanite, Group-IV minerals Mineralogical Magazine, 2008, 72, 1207-1228 |
| 9015456 | CIF | Al8.217 B3.402 Ca0.023 Cl0.001 F0.161 Fe0.042 H3.832 Li0.63 Mn0.087 Na0.541 O30.838 Si5.454 | R 3 m :H | 15.792; 15.792; 7.0878 90; 90; 120 | 1530.79 | Schreyer, W.; Hughes, J. M.; Bernhardt, H. J.; Kalt, A.; Prowatke, S.; Ertl, A. Reexamination of olenite from the type locality: detection of boron in tetrahedral coordination Note: z-coordinate for AlY and y-coordinate for H were altered by Hughes, Aug 2003 European Journal of Mineralogy, 2002, 14, 935-942 |
| 9015460 | CIF | C Ca O3 | R -3 c :H | 4.9742; 4.9742; 17.4676 90; 90; 120 | 374.292 | Antao, S. M.; Hassan, I. Temperature dependence of the structural parameters in the transformation of aragonite to calcite, as determined from in situ synchrotron powder X-ray-diffraction data Note: T = 702 C Note: P = 101 kPa The Canadian Mineralogist, 2010, 48, 1225-1236 |
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