Crystallography Open Database
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Result: there are 88 entries in the selection
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Searching journal of publication like 'American Mineralogist' volume of publication is 81
COD ID | Links | Formula | Space group | Cell parameters | Cell volume | Bibliography |
---|---|---|---|---|---|---|
9015396 | CIF | Fe2 Mn3 O12 Si3 | I a -3 d | 11.8288; 11.8288; 11.8288 90; 90; 90 | 1655.09 | Ottonello, G.; Borketa, M.; Sciuto, P. F. Parameterization of energy and interactions in garnets: End-member properties American Mineralogist, 1996, 81, 429-447 |
9015199 | CIF | Cl2 F12 Pb7 | P -6 | 10.267; 10.267; 3.9844 90; 90; 120 | 363.731 | Merlino, S.; Pasero, M.; Perchiazzi, N.; Kampf, A. R. Laurelite: Its crystal structure and relationship to alpha-PbF2 Note: Re-examination of the crystal by H Yang and A Kampf showed that it was twinned, and the partially occupied sites were relicts. American Mineralogist, 1996, 81, 1277-1281 |
9015042 | CIF | H14 O14 S Zn4 | P -3 | 8.33; 8.33; 10.54 90; 90; 120 | 633.375 | Groat, L. A. The crystal structure of namuwite, a mineral with Zn in tetrahedral and octahedral coordination, and its relationship to the synthetic basic zinc sulfates Note: U(1,2) for S has been changed to match symmetry constraints. American Mineralogist, 1996, 81, 238-243 |
9014905 | CIF | Cl F6 Pb3.5 | P -6 | 10.267; 10.267; 3.9844 90; 90; 120 | 363.731 | Merlino, S.; Pasero, M.; Perchiazzi, N.; Kampf, A. R. Laurelite: Its crystal structure and relationship to alpha-PbF2 American Mineralogist, 1996, 81, 1277-1281 |
9001794 | CIF | Ca O5 Si Ti | A 1 2/a 1 | 6.8912; 8.6234; 6.4065 90; 113.057; 90 | 350.297 | Kunz, M.; Xirouchakis, D.; Lindsley, D. H.; Hausermann, D. High-pressure phase transition in titanite (CaTiOSiO4) Sample: at 6.95 GPa Note: this is a not titanite but instead is a high-pressure polymorph of Ca, transfomred by pressure acting on titanite American Mineralogist, 1996, 81, 1527-1530 |
9001793 | CIF | Mg Ni O4 Si | P b n m | 4.7322; 10.1453; 5.9309 90; 90; 90 | 284.74 | Chen, J.; Li, R.; Parise, J. B.; Weidner, D. J. Pressure-induced ordering in (Ni,Mg)2SiO4 olivine Sample: 4 GPa and 800 C, 109 min American Mineralogist, 1996, 81, 1519-1522 |
9001792 | CIF | Mg Ni O4 Si | P b n m | 4.733; 10.1452; 5.9303 90; 90; 90 | 284.757 | Chen, J.; Li, R.; Parise, J. B.; Weidner, D. J. Pressure-induced ordering in (Ni,Mg)2SiO4 olivine Sample: 4 GPa and 800 C, 63 min American Mineralogist, 1996, 81, 1519-1522 |
9001791 | CIF | Mg Ni O4 Si | P b n m | 4.7325; 10.1454; 5.9313 90; 90; 90 | 284.78 | Chen, J.; Li, R.; Parise, J. B.; Weidner, D. J. Pressure-induced ordering in (Ni,Mg)2SiO4 olivine Sample: 4 GPa and 800 C, 40 min American Mineralogist, 1996, 81, 1519-1522 |
9001790 | CIF | Mg Ni O4 Si | P b n m | 4.7362; 10.1682; 5.9401 90; 90; 90 | 286.067 | Chen, J.; Li, R.; Parise, J. B.; Weidner, D. J. Pressure-induced ordering in (Ni,Mg)2SiO4 olivine Sample: Room pressure, 23 C, (800 C quenched) American Mineralogist, 1996, 81, 1519-1522 |
9001789 | CIF | Al2.15 Ba0.24 H10 K0.01 O21 Si5.85 Sr0.67 | P -1 | 6.785; 17.546; 7.74 89.98; 94.25; 90.06 | 918.91 | Akizuki, M.; Kudoh, Y.; Kuribayashi, T. Crystal structures of the {011}, {610}, and {010} growth sectors in brewsterite Sample: {010} sector American Mineralogist, 1996, 81, 1501-1506 |
9001788 | CIF | Al2.15 Ba0.55 H10 K0.01 O21 Si5.85 Sr0.4 | P -1 | 6.779; 17.53; 7.75 89.98; 94.49; 90.13 | 918.149 | Akizuki, M.; Kudoh, Y.; Kuribayashi, T. Crystal structures of the {011}, {610}, and {010} growth sectors in brewsterite Sample: {610} sector American Mineralogist, 1996, 81, 1501-1506 |
9001787 | CIF | Al2.05 Ba0.45 H10 K0.01 O21 Si5.95 Sr0.5 | P -1 | 6.786; 17.517; 7.742 89.85; 94.07; 90.12 | 917.969 | Akizuki, M.; Kudoh, Y.; Kuribayashi, T. Crystal structures of the {011}, {610}, and {010} growth sectors in brewsterite Sample: {011} sector American Mineralogist, 1996, 81, 1501-1506 |
9001786 | CIF | Ni O18 Sb2 | P 3 | 16.045; 16.045; 9.784 90; 90; 120 | 2181.36 | Bonazzi, P.; Mazzi, F. Bottinoite, Ni(H2O)6[Sb(OH)6]2: Crystal structure, twinning and hydrogen-bond model Sample: BN1, natural Locality: Bottino mine, Apuan Alps, Italy Note: U(1,2) for Sb5 and Sb6 changed to match symmetry constraints. American Mineralogist, 1996, 81, 1494-1500 |
9001785 | CIF | Ni O18 Sb2 | P 3 | 16.06; 16.06; 9.792 90; 90; 120 | 2187.22 | Bonazzi, P.; Mazzi, F. Bottinoite, Ni(H2O)6[Sb(OH)6]2: Crystal structure, twinning and hydrogen-bond model Sample: BS2, synthetic Note: U(1,2) for Sb1 and Sb3 changed to match symmetry constraints. American Mineralogist, 1996, 81, 1494-1500 |
9001784 | CIF | Al2 O8 Pb0.5 Si2 | I 1 2/c 1 | 8.388; 13.067; 14.327 90; 115.19; 90 | 1420.99 | Benna, P.; Tribaudino, M.; Bruno, E. The structure of ordered and disordered lead feldspar (PbAl2Si2O8) Sample: ordered American Mineralogist, 1996, 81, 1337-1343 |
9001783 | CIF | Al O4 Pb0.5 Si | C 1 2/m 1 | 8.428; 13.054; 7.174 90; 115.32; 90 | 713.454 | Benna, P.; Tribaudino, M.; Bruno, E. The structure of ordered and disordered lead feldspar (PbAl2Si2O8) Sample: disordered American Mineralogist, 1996, 81, 1337-1343 |
9001782 | CIF | Cl F6 Pb7 | P -6 | 10.267; 10.267; 3.9844 90; 90; 120 | 363.731 | Merlino, S.; Pasero, M.; Perchiazzi, N.; Kampf, A. R. Laurelite: Its crystal structure and relationship to alpha-PbF2 American Mineralogist, 1996, 81, 1277-1281 |
9001781 | CIF | As0.38 H4 Mn2 O9 V1.62 | P 1 21/n 1 | 7.809; 14.554; 6.705 90; 93.27; 90 | 760.797 | Brugger, J.; Berlepsch, P. Description and crystal structure of fianelite, Mn2V(V,As)O7.2H2O, a new mineral from Fianel, Val Ferrera, Graubunden, Switzerland American Mineralogist, 1996, 81, 1270-1276 |
9001780 | CIF | Ca2 H2 Mg5 O24 Si8 | C 1 2/m 1 | 9.8356; 18.0557; 5.2785 90; 104.782; 90 | 906.377 | Yang, H.; Evans, B. W. X-ray structure refinements of tremolite at 140 and 295 K: Crystal chemistry and petrologic implications T = 295 K American Mineralogist, 1996, 81, 1117-1125 |
9001779 | CIF | Ca2 H2 Mg5 O24 Si8 | C 1 2/m 1 | 9.8293; 18.0307; 5.2752 90; 104.846; 90 | 903.71 | Yang, H.; Evans, B. W. X-ray structure refinements of tremolite at 140 and 295 K: Crystal chemistry and petrologic implications T = 140 K American Mineralogist, 1996, 81, 1117-1125 |
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