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 |
|---|---|---|---|---|---|---|
| 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 |
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