Crystallography Open Database
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Result: there are 474 entries in the selection
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Searching journal of publication like 'American Mineralogist' volume of publication is 89
COD ID  |
Links | Formula |
Space group  |
Cell parameters | Cell volume |
Bibliography |
|---|---|---|---|---|---|---|
| 9003556 | CIF | H3 Mg5 Na3 O24 Si8 | C -1 | 9.883; 54.082; 5.277 90.045; 103.068; 89.96 | 2747.47 | Camara, F.; Oberti, R.; Della Ventura, G.; Welch, M. D.; Maresch, W. V. The crystal structure of synthetic NaNa2Mg5Si8O21(OH)3, a triclinic C-1 amphibole with a triple-cell and H excess Note: occupancies unreported, so calculated formula has an extra OH American Mineralogist, 2004, 89, 1464-1473 |
| 1528651 | CIF | Al2 H1.42 Mg6 Na0.58 O18 Si4 | C 1 | 5.358; 9.281; 14.574 90; 97.08; 90 | 719.204 | Krivovichev, S.V.; Burns, P.C.; Armbruster, T.; Seredkin, M.V.; Organova, N.I.; Chukanov, N.V. Incorporation of sodium into the chlorite structure: the crystal structure of glagolevite, Na (Mg, Al)6 [Si3 Al O10] (O H, O)8 American Mineralogist, 2004, 89, 1138-1141 |
| 9003507 | CIF | H2 Mg2 Na0.193 O6 Si1.333 | C 1 | 5.358; 9.281; 14.574 90; 97.08; 90 | 719.204 | Krivovichev, S. V.; Armbruster, T.; Organova, N. I.; Burns, P. C.; Seredkin, M. V.; Chukanov, N. V. Incorporation of sodium into the chlorite structure: the crystal structure of glagolevite, Na(Mg,Al)6[Si3AlO10](OH,O)8 American Mineralogist, 2004, 89, 1138-1141 |
| 9003111 | CIF | Ca0.15 Mg1.85 O6 Si2 | C 1 2/c 1 | 9.291; 8.679; 4.963 90; 102.22; 90 | 391.132 | Nestola, F.; Tribaudino, M.; Ballaran, T. B. High pressure behavior, transformation and crystal structure of synthetic iron-free pigeonite Sample: P = 6.2 GPa American Mineralogist, 2004, 89, 189-196 |
| 9003317 | CIF | H7.79 O25 Pb3 U6 | C 1 2/c 1 | 28.355; 11.99; 13.998 90; 104.248; 90 | 4612.6 | Brugger, J.; Krivovichev, S. V.; Berlepsch, P.; Meisser, N.; Ansermet, S.; Armbruster, T. Spriggite, Pb3[(UO2)6O8(OH)2](H2O)3, a new mineral with beta-U3O8 - type sheets: Description and crystal structure American Mineralogist, 2004, 89, 339-347 |
| 9003382 | CIF | Mg O3 Si | C 1 2/c 1 | 7.394; 6; 3.464 90; 117.9; 90 | 135.814 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 240 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003383 | CIF | Mg O3 Si | C 1 2/c 1 | 7.565; 6.51; 3.759 90; 115.8; 90 | 166.67 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 220 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003384 | CIF | Mg O3 Si | C 1 2/c 1 | 7.608; 6.823; 3.939 90; 113.4; 90 | 187.654 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 200 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003385 | CIF | Mg O3 Si | C 1 2/c 1 | 7.526; 6.928; 4 90; 110.8; 90 | 194.968 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 180 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003386 | CIF | Mg O3 Si | C 1 2/c 1 | 7.326; 6.823; 3.939 90; 107.7; 90 | 187.572 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 160 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003387 | CIF | Mg O3 Si | C 1 2/c 1 | 7.023; 6.51; 3.759 90; 104.1; 90 | 166.683 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 140 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003388 | CIF | Mg O3 Si | C 1 2/c 1 | 6.6332; 6; 3.464 90; 100; 90 | 135.77 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 120 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
| 9003389 | CIF | Ca Mg O6 Si2 | C 1 2/c 1 | 9.756; 9.067; 5.235 90; 108.7; 90 | 438.63 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model diopside after Cameron et al. (1973) with O3-O3-O3 angle = 166.4 and model oxygen radius = 1.318 American Mineralogist, 2004, 89, 614-628 |
| 9003390 | CIF | Ca Mg O6 Si2 | C 1 2/c 1 | 9.876; 9.17; 5.294 90; 109; 90 | 453.32 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model diopside at 1000C after Cameron et al. (1973) with O3-O3-O3 angle = 168.5 and model oxygen radius = 1.330 American Mineralogist, 2004, 89, 614-628 |
| 9003391 | CIF | Ca Mg O6 Si2 | C 1 2/c 1 | 9.76; 9.071; 5.237 90; 108.7; 90 | 439.171 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model diopside after Levien and Prewitt (1981) with O3-O3-O3 angle = 166.4 and model oxygen radius = 1.319 American Mineralogist, 2004, 89, 614-628 |
| 9003392 | CIF | Ca Mg O6 Si2 | C 1 2/c 1 | 9.607; 8.939; 5.161 90; 108.3; 90 | 420.796 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model diopside at 5.3 GPa after Levien and Prewitt (1981) with O3-O3-O3 angle = 163.6 and model oxygen radius = 1.304 American Mineralogist, 2004, 89, 614-628 |
| 9003393 | CIF | Fe O3 Si | C 1 2/c 1 | 9.552; 8.844; 5.106 90; 103.8; 90 | 418.893 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model ferrosilite at 1.87 GPa after Hugh-Jones et al. (1995) with O3-O3-O3 angle = 138.3 and model oxygen radius = 1.366 American Mineralogist, 2004, 89, 614-628 |
| 9003394 | CIF | Cr Na O6 Si2 | C 1 2/c 1 | 9.653; 8.944; 5.164 90; 109.6; 90 | 420.008 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model kosmochlor after Cameron et al. (1973) with O3-O3-O3 angle = 172.0 and model oxygen radius = 1.294 American Mineralogist, 2004, 89, 614-628 |
| 9003395 | CIF | Cr Na O6 Si2 | C 1 2/c 1 | 9.697; 8.98; 5.184 90; 109.7; 90 | 424.997 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model kosmochlor at 600C after Cameron et al. (1973) with O3-O3-O3 angle = 172.9 and model oxygen radius = 1.299 American Mineralogist, 2004, 89, 614-628 |
| 9003396 | CIF | Cr Na O6 Si2 | C 1 2/c 1 | 9.65; 8.937; 5.16 90; 109.7; 90 | 418.963 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model kosmochlor after Origlieri et al. (2003) with O3-O3-O3 angle = 172.8 and model oxygen radius = 1.292 American Mineralogist, 2004, 89, 614-628 |
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