Crystallography Open Database
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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 |
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9003428 | CIF | Mg O3 Si | P b c a | 18.535; 9.024; 5.21 90; 90; 90 | 871.424 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthoenstatite at 1360 K after Yang and Ghose (1995) with O3A-O3A-O3A angle = 163.0, O3B-O3B-O3B angle = 149.5, and model oxygen radius = 1.317 American Mineralogist, 2004, 89, 614-628 |
9003429 | CIF | Mg O3 Si | P b c a | 18.363; 8.864; 5.118 90; 90; 90 | 833.055 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthoenstatite after Hugh-Jones and Angel (1994) with O3A-O3A-O3A angle = 158.7, O3B-O3B-O3B angle = 139.0, and model oxygen radius = 1.302 American Mineralogist, 2004, 89, 614-628 |
9003430 | CIF | Mg O3 Si | P b c a | 18.027; 8.683; 5.013 90; 90; 90 | 784.677 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthoenstatite at 8.10 GPa after Hugh-Jones and Angel (1994) with O3A-O3A-O3A angle = 158.5, O3B-O3B-O3B angle = 136.4, and model oxygen radius = 1.276 American Mineralogist, 2004, 89, 614-628 |
9003431 | CIF | Mg O3 Si | P b c n | 7.037; 6.928; 4 90; 90; 90 | 195.009 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model protopyroxene 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 |
9003432 | CIF | Mg O3 Si | P b c n | 9.268; 9.102; 5.255 90; 90; 90 | 443.298 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model protoenstatite at 1360 K after Yang and Ghose (1995) with O3-O3-O3 angle = 168.4 and model oxygen radius = 1.321 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
9003433 | CIF | Mg O3 Si | P b c n | 9.199; 9.026; 5.211 90; 90; 90 | 432.67 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model protopyroxene after Yang et al. (1999) with O3-O3-O3 angle = 166.2 and model oxygen radius = 1.312 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
9003434 | CIF | Mg O3 Si | P b c n | 9.154; 8.981; 5.185 90; 90; 90 | 426.27 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model protopyroxene after Yang et al. (1999) with O3-O3-O3 angle = 165.9 and model oxygen radius = 1.306 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
9003435 | CIF | Mg O3 Si | P 21 c n | 6.532; 6; 3.464 90; 90; 90 | 135.761 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model hi-P protopx with O3A-O3A-O3A angle = 120, O3B-O3B-O3B 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 |
9003436 | CIF | Mg O3 Si | P 21 c n | 9.127; 8.877; 5.125 90; 90; 90 | 415.229 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model hi-P protopx at 2.50 GPa after Yang et al. (1999) with O3A-O3A-O3A angle = 154.0, O3B-O3B-O3B angle = 212.1, and model oxygen radius = 1.315 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
9003437 | CIF | Mg O3 Si | P 21 c n | 9.002; 8.698; 5.022 90; 90; 90 | 393.22 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model hi-P protopx at 9.98 GPa after Yang et al. (1999) with O3A-O3A-O3A angle = 147.8, O3B-O3B-O3B angle = 220.8, and model oxygen radius = 1.307 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience American Mineralogist, 2004, 89, 614-628 |
9003456 | CIF | Mg O3 Si | P b n m | 4.778; 4.9298; 6.899 90; 90; 90 | 162.503 | Dobson, D. P.; Jacobsen, S. D. The flux growth of magnesium silicate perovskite single crystals American Mineralogist, 2004, 89, 807-811 |
9003407 | CIF | Mn Na O6 Si2 | C 1 2/c 1 | 9.698; 8.973; 5.181 90; 109.9; 90 | 423.93 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium manganese px after Ohashi et al. (1987) with O3-O3-O3 angle = 174.1 and model oxygen radius = 1.297 American Mineralogist, 2004, 89, 614-628 |
9003475 | CIF | Mn O2 | P n m a | 9.2734; 2.8638; 4.5219 90; 90; 90 | 120.089 | Post, J. E.; Heaney, P. J. Neutron and synchrotron X-ray diffraction study of the structures and dehydration behaviors of ramsdellite and "groutellite" American Mineralogist, 2004, 89, 969-975 |
9003476 | CIF | Mn O2 | P n m a | 9.5155; 2.8644; 4.7061 90; 90; 90 | 128.27 | Post, J. E.; Heaney, P. J. Neutron and synchrotron X-ray diffraction study of the structures and dehydration behaviors of ramsdellite and "groutellite" American Mineralogist, 2004, 89, 969-975 |
9003410 | CIF | Na O6 Sc Si2 | C 1 2/c 1 | 9.929; 9.189; 5.305 90; 109.8; 90 | 455.401 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium scandium px after Ohashi et al. (1994A) with O3-O3-O3 angle = 173.7 and model oxygen radius = 1.328 American Mineralogist, 2004, 89, 614-628 |
9003409 | CIF | Na O6 Si2 Ti | C 1 2/c 1 | 9.791; 9.06; 5.231 90; 109.9; 90 | 436.316 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium titanium px after Ohashi et al. (1982) with O3-O3-O3 angle = 173.9 and model oxygen radius = 1.310 American Mineralogist, 2004, 89, 614-628 |
9003411 | CIF | Na O6 Si2 V | C 1 2/c 1 | 9.712; 8.992; 5.192 90; 109.7; 90 | 426.881 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium vanadium px with O3-O3-O3 angle = 173.0 and model oxygen radius = 1.300 American Mineralogist, 2004, 89, 614-628 |
9003334 | CIF | O21 Si6 Tm5.902 | P -1 | 6.5499; 6.5876; 17.8916 83.828; 88.368; 88.152 | 766.872 | Fleet, M. E.; Liu, X. A new rare earth disilicate (REE2Si2O7: REE = Dy, Tm, Lu; type-L): Evidence for nonquenchable 10 GPa polymorph with silicon in fivefold trigonal bipyramidal coordination? American Mineralogist, 2004, 89, 396-404 |
9003418 | CIF | O3 Si Zn | C 1 2/c 1 | 9.755; 9.083; 5.244 90; 107.9; 90 | 442.152 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model zinc px after Morimoto et al. (1975) with O3-O3-O3 angle = 161.3 and model oxygen radius = 1.329 American Mineralogist, 2004, 89, 614-628 |
9003478 | CIF | O8 Se2 Sr U | P -1 | 5.6722; 6.7627; 11.2622 104.698; 93.708; 109.489 | 388.615 | Almond, P. M.; Albrecht-Schmitt T E Hydrothermal synthesis and crystal chemistry of the new strontium uranyl selenites, Sr[(UO2)3(SeO3)2O2].4H2O and Sr[(UO2)(SeO3)2].2H2O American Mineralogist, 2004, 89, 976-980 |
9003459 | CIF | S3 Sb2 | P n m a | 11.282; 3.8296; 11.225 90; 90; 90 | 484.982 | Kyono, A.; Kimata, M. Structural variations induced by difference of the inert pair effect in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3 Sample #1 American Mineralogist, 2004, 89, 932-940 |
9003460 | CIF | S3 Sb2 | P n m a | 11.311; 3.8389; 11.223 90; 90; 90 | 487.323 | Kyono, A.; Kimata, M. Structural variations induced by difference of the inert pair effect in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3 Sample #2 American Mineralogist, 2004, 89, 932-940 |
9003461 | CIF | S3 Sb2 | P n m a | 11.2845; 3.822; 11.203 90; 90; 90 | 483.178 | Kyono, A.; Kimata, M. Structural variations induced by difference of the inert pair effect in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3 Sample #3 American Mineralogist, 2004, 89, 932-940 |
9003462 | CIF | S3 Sb2 | P n m a | 11.3197; 3.8332; 11.233 90; 90; 90 | 487.407 | Kyono, A.; Kimata, M. Structural variations induced by difference of the inert pair effect in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3 Sample #4 American Mineralogist, 2004, 89, 932-940 |
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