Crystallography Open Database

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Searching journal of publication like 'American Mineralogist' volume of publication is 89

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9003459 CIFS3 Sb2P n m a11.282; 3.8296; 11.225
90; 90; 90
484.982Kyono, 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 CIFS3 Sb2P n m a11.311; 3.8389; 11.223
90; 90; 90
487.323Kyono, 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 CIFS3 Sb2P n m a11.2845; 3.822; 11.203
90; 90; 90
483.178Kyono, 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 CIFS3 Sb2P n m a11.3197; 3.8332; 11.233
90; 90; 90
487.407Kyono, 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
9003478 CIFO8 Se2 Sr UP -15.6722; 6.7627; 11.2622
104.698; 93.708; 109.489
388.615Almond, 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
9003418 CIFO3 Si ZnC 1 2/c 19.755; 9.083; 5.244
90; 107.9; 90
442.152Thompson, 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
9003334 CIFO21 Si6 Tm5.902P -16.5499; 6.5876; 17.8916
83.828; 88.368; 88.152
766.872Fleet, 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
9003411 CIFNa O6 Si2 VC 1 2/c 19.712; 8.992; 5.192
90; 109.7; 90
426.881Thompson, 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
9003409 CIFNa O6 Si2 TiC 1 2/c 19.791; 9.06; 5.231
90; 109.9; 90
436.316Thompson, 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
9003410 CIFNa O6 Sc Si2C 1 2/c 19.929; 9.189; 5.305
90; 109.8; 90
455.401Thompson, 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
9003475 CIFMn O2P n m a9.2734; 2.8638; 4.5219
90; 90; 90
120.089Post, 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 CIFMn O2P n m a9.5155; 2.8644; 4.7061
90; 90; 90
128.27Post, 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
9003407 CIFMn Na O6 Si2C 1 2/c 19.698; 8.973; 5.181
90; 109.9; 90
423.93Thompson, 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
9003382 CIFMg O3 SiC 1 2/c 17.394; 6; 3.464
90; 117.9; 90
135.814Thompson, 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 CIFMg O3 SiC 1 2/c 17.565; 6.51; 3.759
90; 115.8; 90
166.67Thompson, 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 CIFMg O3 SiC 1 2/c 17.608; 6.823; 3.939
90; 113.4; 90
187.654Thompson, 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 CIFMg O3 SiC 1 2/c 17.526; 6.928; 4
90; 110.8; 90
194.968Thompson, 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 CIFMg O3 SiC 1 2/c 17.326; 6.823; 3.939
90; 107.7; 90
187.572Thompson, 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 CIFMg O3 SiC 1 2/c 17.023; 6.51; 3.759
90; 104.1; 90
166.683Thompson, 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 CIFMg O3 SiC 1 2/c 16.6332; 6; 3.464
90; 100; 90
135.77Thompson, 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

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