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 |
|---|---|---|---|---|---|---|
| 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 |
| 9003397 | CIF | Cr Na O6 Si2 | C 1 2/c 1 | 9.401; 8.738; 5.045 90; 108.7; 90 | 392.549 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model kosmochlor at 9.28 GPa after Origlieri et al. (2003) with O3-O3-O3 angle = 166.1 and model oxygen radius = 1.271 American Mineralogist, 2004, 89, 614-628 |
| 9003398 | CIF | Al Li O6 Si2 | C 1 2/c 1 | 9.57; 8.717; 5.033 90; 112.1; 90 | 389.014 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model spodumene after Cameron et al. (1973) with O3-O3-O3 angle = 189.5 and model oxygen radius = 1.263 American Mineralogist, 2004, 89, 614-628 |
| 9003399 | CIF | Al Li O6 Si2 | C 1 2/c 1 | 9.589; 8.766; 5.061 90; 111.7; 90 | 395.265 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model spodumene at 760C after Cameron et al. (1973) with O3-O3-O3 angle = 186.6 and model oxygen radius = 1.267 American Mineralogist, 2004, 89, 614-628 |
| 9003400 | CIF | Al Li O6 Si2 | C 1 2/c 1 | 9.572; 8.715; 5.032 90; 112.1; 90 | 388.928 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model spodumene after Arlt and Angel (2003) with O3-O3-O3 angle = 189.9 and model oxygen radius = 1.263 American Mineralogist, 2004, 89, 614-628 |
| 9003401 | CIF | Al Li O6 Si2 | C 1 2/c 1 | 9.503; 8.655; 4.997 90; 112.1; 90 | 380.799 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model spodumene at 3.164 GPa after Arlt and Angel (2003) with O3-O3-O3 angle = 189.5 and model oxygen radius = 1.254 American Mineralogist, 2004, 89, 614-628 |
| 9003402 | CIF | Fe Li O6 Si2 | C 1 2/c 1 | 9.695; 8.919; 5.149 90; 110.9; 90 | 415.938 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model lithium iron px after Redhammer et al. (2001) with O3-O3-O3 angle = 180.8 and model oxygen radius = 1.287 American Mineralogist, 2004, 89, 614-628 |
| 9003403 | CIF | Ga Li O6 Si2 | C 1 2/c 1 | 9.601; 8.839; 5.103 90; 110.7; 90 | 405.101 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model lilthium gallium px after Sato et al. (1994) with O3-O3-O3 angle = 179.9 and model oxygen radius = 1.276 American Mineralogist, 2004, 89, 614-628 |
| 9003404 | CIF | Li O6 Si2 V | C 1 2/c 1 | 9.648; 8.898; 5.137 90; 110.5; 90 | 413.073 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model lithium vanadium px after Satto et al. (1997) with O3-O3-O3 angle = 178.1 and model oxygen radius = 1.284 American Mineralogist, 2004, 89, 614-628 |
| 9003405 | CIF | Li O6 Sc Si2 | C 1 2/c 1 | 9.838; 9.092; 5.249 90; 110.1; 90 | 440.912 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model lithium scandium px after Hawthorne and Grundy (1977) with O3-O3-O3 angle = 175.6 and model oxygen radius = 1.313 American Mineralogist, 2004, 89, 614-628 |
| 9003406 | CIF | Al Na O6 Si2 | C 1 2/c 1 | 9.527; 8.81; 5.087 90; 110; 90 | 401.217 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model jadeite after Clark et al. (1969) with O3-O3-O3 angle = 174.7 and model oxygen radius = 1.273 American Mineralogist, 2004, 89, 614-628 |
| 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 |
| 9003408 | CIF | Fe Na O6 Si2 | C 1 2/c 1 | 9.737; 9.009; 5.201 90; 109.9; 90 | 428.992 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model acmite after Cameron et al. (1973) with O3-O3-O3 angle = 174.0 and model oxygen radius = 1.302 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 |
| 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 |
| 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 |
| 9003412 | CIF | Ga Na O6 Si2 | C 1 2/c 1 | 9.64; 8.928; 5.155 90; 109.7; 90 | 417.702 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium gallium px after Ohashi et al. (1995) with O3-O3-O3 angle = 172.7 and model oxygen radius = 1.291 American Mineralogist, 2004, 89, 614-628 |
| 9003413 | CIF | In Na O6 Si2 | C 1 2/c 1 | 9.967; 9.241; 5.335 90; 109.4; 90 | 463.481 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model sodium indium px after Ohashi et al. (1990) with O3-O3-O3 angle = 171.0 and model oxygen radius = 1.338 American Mineralogist, 2004, 89, 614-628 |
| 9003414 | CIF | Ca Ni O6 Si2 | C 1 2/c 1 | 9.724; 9.043; 5.221 90; 108.5; 90 | 435.379 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model calcium nickel px after Ghose et al. (1987) with O3-O3-O3 angle = 165.2 and model oxygen radius = 1.316 American Mineralogist, 2004, 89, 614-628 |
| 9003415 | CIF | Ca Co O6 Si2 | C 1 2/c 1 | 9.785; 9.1; 5.254 90; 108.5; 90 | 443.659 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model calcium cobalt px after Ghose et al. (1987) with O3-O3-O3 angle = 165.1 and model oxygen radius = 1.325 American Mineralogist, 2004, 89, 614-628 |
| 9003416 | CIF | Ca Fe O6 Si2 | C 1 2/c 1 | 9.828; 9.142; 5.278 90; 108.4; 90 | 449.972 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model hedenbergite after Zhang et al. (1997) with O3-O3-O3 angle = 164.4 and model oxygen radius = 1.332 American Mineralogist, 2004, 89, 614-628 |
| 9003417 | CIF | Ca Mn O6 Si2 | C 1 2/c 1 | 9.94; 9.248; 5.339 90; 108.3; 90 | 465.967 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model johannsenite after Freed and Peacor (1967) with O3-O3-O3 angle = 163.8 and model oxygen radius = 1.348 American Mineralogist, 2004, 89, 614-628 |
| 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 |
| 9003315 | CIF | Al1.74 Ba0.09 F0.02 Fe0.21 H1.98 K0.91 Mg0.93 Mn1.53 O11.98 Si2.56 Ti0.03 | C 1 2/m 1 | 5.3791; 9.319; 10.2918 90; 100.186; 90 | 507.774 | Ishida, K.; Hawthorne, F. C.; Hirowatari, F. Shirozulite, KMn3(Si3Al)O10(OH)2, a new manganese-dominant trioctahedral mica: Description and crystal structure Note: Displacement factors for O1, O2 and O4 have been altered. American Mineralogist, 2004, 89, 232-238 |
| 9003444 | CIF | Al1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72 | C 1 2/m 1 | 5.337; 9.24; 10.237 90; 100.02; 90 | 497.126 | Comodi, P.; Fumagalli, P.; Montagnoli, M.; Zanazzi, P. F. A single-crystal study on the pressure behavior of phlogopite and petrological implications P = 0.0001 GPa American Mineralogist, 2004, 89, 647-653 |
| 9003445 | CIF | Al1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72 | C 1 2/m 1 | 5.318; 9.21; 10.1 90; 100.12; 90 | 486.989 | Comodi, P.; Fumagalli, P.; Montagnoli, M.; Zanazzi, P. F. A single-crystal study on the pressure behavior of phlogopite and petrological implications P = 1.2 GPa American Mineralogist, 2004, 89, 647-653 |
| 9003446 | CIF | Al1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72 | C 1 2/m 1 | 5.291; 9.16; 9.9 90; 100.3; 90 | 472.077 | Comodi, P.; Fumagalli, P.; Montagnoli, M.; Zanazzi, P. F. A single-crystal study on the pressure behavior of phlogopite and petrological implications P = 3.2 GPa American Mineralogist, 2004, 89, 647-653 |
| 9003447 | CIF | Al1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72 | C 1 2/m 1 | 5.271; 9.13; 9.78 90; 100.3; 90 | 463.07 | Comodi, P.; Fumagalli, P.; Montagnoli, M.; Zanazzi, P. F. A single-crystal study on the pressure behavior of phlogopite and petrological implications P = 5.0 GPa American Mineralogist, 2004, 89, 647-653 |
| 9003448 | CIF | Al1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72 | C 1 2/m 1 | 5.256; 9.105; 9.71 90; 100.4; 90 | 457.047 | Comodi, P.; Fumagalli, P.; Montagnoli, M.; Zanazzi, P. F. A single-crystal study on the pressure behavior of phlogopite and petrological implications P = 6.0 GPa American Mineralogist, 2004, 89, 647-653 |
| 9003457 | CIF | Al0.1 Ca0.06 F0.47 Fe2.63 H1.51 K0.125 Li1.66 Mg1.35 Mn0.13 Na1.376 O23.51 Si8 Ti0.06 Zn0.31 | C 1 2/m 1 | 9.535; 17.876; 5.294 90; 102.54; 90 | 880.824 | Oberti, R.; Camara, F.; Caballero, J. M. Ferri-ottoliniite and ferriwhittakerite, two new end-members of the new Group 5 for monoclinic amphiboles American Mineralogist, 2004, 89, 888-893 |
| 9003458 | CIF | Al0.1 Ca0.11 F0.7 Fe2.06 H1.3 K0.232 Li1.35 Mg1.47 Mn0.12 Na2.411 O23.3 Si8 Ti0.12 Zn0.4 | C 1 2/m 1 | 9.712; 17.851; 5.297 90; 103.63; 90 | 892.473 | Oberti, R.; Camara, F.; Caballero, J. M. Ferri-ottoliniite and ferriwhittakerite, two new end-members of the new Group 5 for monoclinic amphiboles American Mineralogist, 2004, 89, 888-893 |
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