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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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 |
9003419 | CIF | Mg O3 Si | P 1 21/c 1 | 6.928; 6; 3.464 90; 109.47; 90 | 135.758 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinopx, closest-packed, ABABCACABCBC, with O3A-O3A-O3A angle = 240, O3B-O3B-O3B angle = 120, and model oxygen radius = 1 American Mineralogist, 2004, 89, 614-628 |
9003420 | CIF | Mg O3 Si | P 1 21/c 1 | 7.559; 6.928; 4 90; 105.3; 90 | 202.051 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinopx with O3A-O3A-O3A angle = 180, O3B-O3B-O3B angle = 120, and model oxygen radius = 1 American Mineralogist, 2004, 89, 614-628 |
9003421 | CIF | Mg O3 Si | P 1 21/c 1 | 9.725; 8.872; 5.122 90; 108.9; 90 | 418.101 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinoenstatite after Pannhorst (1984) with O3A-O3A-O3A angle = 202.8, O3B-O3B-O3B angle = 138.1, and model oxygen radius = 1.306 American Mineralogist, 2004, 89, 614-628 |
9003422 | CIF | Mg O3 Si | P 1 21/c 1 | 9.764; 8.953; 5.169 90; 108.8; 90 | 427.752 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinoenstatite at 700C after Pannhorst (1984) with O3A-O3A-O3A angle = 197.1, O3B-O3B-O3B angle = 141.6, and model oxygen radius = 1.307 American Mineralogist, 2004, 89, 614-628 |
9003423 | CIF | Al Li O6 Si2 | P 1 21/c 1 | 9.402; 8.587; 4.958 90; 110.2; 90 | 375.664 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinospodumene at P = 3.342 GPa after Arlt and Angel (2000) with O3A-O3A-O3A angle = 203.2, O3B-O3B-O3B angle = 152.5, and model oxygen radius = 1.265 American Mineralogist, 2004, 89, 614-628 |
9003424 | CIF | Al Li O6 Si2 | P 1 21/c 1 | 9.292; 8.459; 4.884 90; 109.6; 90 | 361.644 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model low clinospodumene at P = 8.835 GPa after Arlt and Angel (2000) with O3A-O3A-O3A angle = 206.4, O3B-O3B-O3B angle = 143.5, and model oxygen radius = 1.254 American Mineralogist, 2004, 89, 614-628 |
9003425 | CIF | Mg O3 Si | P b c a | 14.58; 6.928; 4 90; 90; 90 | 404.041 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthopx with O3A-O3A-O3A angle = 180, O3B-O3B-O3B 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 |
9003426 | CIF | Mg O3 Si | P b c a | 14.074; 6.928; 4 90; 90; 90 | 390.019 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthopx with O3A-O3A-O3A angle = 180, O3B-O3B-O3B 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 |
9003427 | CIF | Mg O3 Si | P b c a | 18.363; 8.867; 5.119 90; 90; 90 | 833.5 | Thompson, R. M.; Downs, R. T. Model pyroxenes II: Structural variation as a function of tetrahedral rotation model orthoenstatite after Yang and Ghose (1995) with O3A-O3A-O3A angle = 158.9, O3B-O3B-O3B angle = 139.3, and model oxygen radius = 1.302 American Mineralogist, 2004, 89, 614-628 |
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 |
9003438 | CIF | Ca4.32 F Mn0.68 O12 P3 | P 63/m | 9.3429; 9.3429; 6.811 90; 90; 120 | 514.879 | Hughes, John M.; Ertl, Andreas; Bernhardt, Heinz-Jürgen; Rossman, George R.; Rakovan, John F. Mn-rich fluorapatite from Austria: Crystal structure, chemical analysis, and spectroscopic investigations American Mineralogist, 2004, 89, 629-632 |
9003439 | CIF | Al1.96 Ba0.94 H8 O13.54 Si3.04 | P -4 21 m | 9.5909; 9.5909; 6.5339 90; 90; 90 | 601.023 | Gatta, G. D.; Ballaran, T. B.; Comodi, P.; Zanazzi, P. F. Isothermal equation of state and compressional behavior of tetragonal edingtonite Sample at P = 0.0001 GPa in air American Mineralogist, 2004, 89, 633-639 |
9003440 | CIF | Al1.96 Ba0.91 H8 O13.32 Si3.04 | P -4 21 m | 9.5909; 9.5909; 6.5339 90; 90; 90 | 601.023 | Gatta, G. D.; Ballaran, T. B.; Comodi, P.; Zanazzi, P. F. Isothermal equation of state and compressional behavior of tetragonal edingtonite Sample at P = 0.0001 GPa in diamond cell American Mineralogist, 2004, 89, 633-639 |
9003441 | CIF | Al1.96 Ba0.88 H8 O13.32 Si3.04 | P -4 21 m | 9.4669; 9.4669; 6.4765 90; 90; 90 | 580.438 | Gatta, G. D.; Ballaran, T. B.; Comodi, P.; Zanazzi, P. F. Isothermal equation of state and compressional behavior of tetragonal edingtonite Sample at P = 2.285 GPa American Mineralogist, 2004, 89, 633-639 |
9003442 | CIF | Al1.96 Ba0.89 H7.68 O13.32 Si3.04 | P -4 21 m | 9.3466; 9.3466; 6.42705 90; 90; 90 | 561.46 | Gatta, G. D.; Ballaran, T. B.; Comodi, P.; Zanazzi, P. F. Isothermal equation of state and compressional behavior of tetragonal edingtonite Sample at P = 4.611 GPa American Mineralogist, 2004, 89, 633-639 |
9003443 | CIF | H2 Mg6 Na2 O24 Si8 | P 1 21/m 1 | 9.689; 17.938; 5.268 90; 102.5; 90 | 893.882 | Iezzi, G.; Della Ventura, G.; Oberti, R.; Camara, F.; Holtz, F. Synthesis and crystal-chemistry of Na(NaMg)Mg5Si8O22(OH)2, a P2_1/m amphibole American Mineralogist, 2004, 89, 640-646 |
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 |
9003449 | CIF | As0.975 S3 Sb1.025 | P 1 21/a 1 | 11.949; 9.028; 10.13 90; 116.15; 90 | 980.926 | Kyono, A.; Kimata, M. Structural reinvestigation of getchellite As0.98Sb1.02S3.00 American Mineralogist, 2004, 89, 696-700 |
9003450 | CIF | B Ca H O5 Si | P 1 21/c 1 | 4.85; 7.627; 9.659 90; 90.255; 90 | 357.292 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: #45837, single crystal data American Mineralogist, 2004, 89, 767-776 |
9003451 | CIF | B1.25 Ca H1.25 O5 Si0.75 | P 1 21/c 1 | 4.8014; 7.578; 9.5419 90; 90.434; 90 | 347.172 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: Refinement of the conventional X-ray data for sample #92735 American Mineralogist, 2004, 89, 767-776 |
9003452 | CIF | B1.25 Ca H1.25 O5 Si0.75 | P 1 21/c 1 | 4.8005; 7.5788; 9.5432 90; 90.437; 90 | 347.191 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: Refinement of the synchrotron data for sample #92735 American Mineralogist, 2004, 89, 767-776 |
9003453 | CIF | B1.25 Ca H1.25 O5 Si0.75 | P 1 21/c 1 | 4.7967; 7.5711; 9.5321 90; 90.427; 90 | 346.161 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: Refinement of the neutron data (RT) for sample #92735 American Mineralogist, 2004, 89, 767-776 |
9003454 | CIF | B1.25 Ca H1.25 O5 Si0.75 | P 1 21/c 1 | 4.7892; 7.5644; 9.5362 90; 90.476; 90 | 345.46 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: Refinement of the neutron data (LT) for sample #92735 American Mineralogist, 2004, 89, 767-776 |
9003455 | CIF | B1.25 Ca H1.25 O5 Si0.75 | P 1 21/c 1 | 4.80042; 7.57864; 9.5426 90; 90.435; 90 | 347.156 | Perchiazzi, N.; Gualtieri, A. F.; Merlino, S.; Kampf, A. R. The atomic structure of bakerite and its relationship to datolite Sample: Combined refinement American Mineralogist, 2004, 89, 767-776 |
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 |
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 |
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 |
9003463 | CIF | Bi0.064 S3 Sb1.936 | P n m a | 11.3122; 3.8428; 11.221 90; 90; 90 | 487.783 | 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: Sb1.935Bi.065S3 American Mineralogist, 2004, 89, 932-940 |
9003464 | CIF | Bi0.364 S3 Sb1.636 | P n m a | 11.274; 3.8739; 11.16 90; 90; 90 | 487.406 | 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: Sb1.637Bi.363S3 American Mineralogist, 2004, 89, 932-940 |
9003465 | CIF | Bi0.516 S3 Sb1.484 | P n m a | 11.318; 3.883; 11.226 90; 90; 90 | 493.358 | 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: Sb1.483Bi.517S3 American Mineralogist, 2004, 89, 932-940 |
9003466 | CIF | Bi0.536 S3 Sb1.464 | P n m a | 11.309; 3.871; 11.1876 90; 90; 90 | 489.761 | 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: Sb1.463Bi.537S3 American Mineralogist, 2004, 89, 932-940 |
9003467 | CIF | Bi0.573 S3 Sb1.427 | P n m a | 11.318; 3.8872; 11.228 90; 90; 90 | 493.98 | 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: Sb1.426Bi.574S3 American Mineralogist, 2004, 89, 932-940 |
9003468 | CIF | Bi1.09 S3 Sb0.91 | P n m a | 11.256; 3.8966; 11.205 90; 90; 90 | 491.453 | 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: Sb.910Bi1.090S3 American Mineralogist, 2004, 89, 932-940 |
9003469 | CIF | Bi1.612 S3 Sb0.388 | P n m a | 11.336; 3.9562; 11.186 90; 90; 90 | 501.664 | 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: Sb0.387Bi1.613S3 American Mineralogist, 2004, 89, 932-940 |
9003470 | CIF | Bi1.638 S3 Sb0.362 | P n m a | 11.31; 3.9526; 11.119 90; 90; 90 | 497.063 | 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: Sb0.362Bi1.638S3 American Mineralogist, 2004, 89, 932-940 |
9003471 | CIF | Bi1.68 S3 Sb0.32 | P n m a | 11.318; 3.9547; 11.1631 90; 90; 90 | 499.652 | 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: Sb0.320Bi1.680S3 American Mineralogist, 2004, 89, 932-940 |
9003472 | CIF | Bi2 S3 | P n m a | 11.316; 3.9709; 11.178 90; 90; 90 | 502.28 | 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 |
9003473 | CIF | Bi2 S3 | P n m a | 11.345; 3.994; 11.193 90; 90; 90 | 507.176 | 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 |
9003474 | CIF | Bi2 S3 | P n m a | 11.354; 3.9911; 11.188 90; 90; 90 | 506.984 | 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 |
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 |
9003477 | CIF | H6.8 O18 Se2 Sr U3 | C 1 2/m 1 | 17.014; 7.0637; 7.1084 90; 100.544; 90 | 839.875 | 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 |
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 |
9003479 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.0834; 8.0834; 8.0834 90; 90; 90 | 528.18 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 273 K and P = 0 GPa, inversion parameter x = .320 American Mineralogist, 2004, 89, 981-986 |
9003480 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.0727; 8.0727; 8.0727 90; 90; 90 | 526.086 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 549 K and P = 0.4 GPa, inversion parameter x = .262 American Mineralogist, 2004, 89, 981-986 |
9003481 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.0874; 8.0874; 8.0874 90; 90; 90 | 528.965 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 757 K and P = 0.4 GPa, inversion parameter x = .292 American Mineralogist, 2004, 89, 981-986 |
9003482 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.1104; 8.1104; 8.1104 90; 90; 90 | 533.491 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 1015 K and P = 1.5 GPa, inversion parameter x = .386 American Mineralogist, 2004, 89, 981-986 |
9003483 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.1274; 8.1274; 8.1274 90; 90; 90 | 536.852 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 1202 K and P = 2.0 GPa, inversion parameter x = .453 American Mineralogist, 2004, 89, 981-986 |
9003484 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.135; 8.135; 8.135 90; 90; 90 | 538.36 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 1363 K and P = 2.8 GPa, inversion parameter x = .571 American Mineralogist, 2004, 89, 981-986 |
9003485 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.1452; 8.1452; 8.1452 90; 90; 90 | 540.387 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 1507 K and P = 3.2 GPa, inversion parameter x = .633 American Mineralogist, 2004, 89, 981-986 |
9003486 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.1171; 8.1171; 8.1171 90; 90; 90 | 534.814 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 1058 K and P = 1.9 GPa, inversion parameter x = .524 American Mineralogist, 2004, 89, 981-986 |
9003487 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.105; 8.105; 8.105 90; 90; 90 | 532.426 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 887 K and P = 1.7 GPa, inversion parameter x = .509 American Mineralogist, 2004, 89, 981-986 |
9003488 | CIF | Al2 Mg O4 | F d -3 m :2 | 8.08; 8.08; 8.08 90; 90; 90 | 527.514 | Meducin, F.; Redfern, S. A. T.; Le Godec, Y.; Stone, H. J.; Tucker, M. G.; Dove, M. T.; Marshall, W. G. Study of cation order-disorder in MgAl2O4 spinel by in situ neutron diffraction up to 1600 K and 3.2 GPa Sample at T = 381 K and P = 0.5 GPa, inversion parameter x = .365 American Mineralogist, 2004, 89, 981-986 |
9003489 | CIF | Al2.42 H8.448 O30.36 Si9.58 | I m m a | 20.291; 23.84; 12.807 90; 90; 90 | 6195.23 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Wat represents an unknown distribution across the Wat sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001,Wat8.06] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-RT, T = 25 C American Mineralogist, 2004, 89, 1033-1042 |
9003490 | CIF | Al2.1 Ca0.67 H4.78 O25.31 Si9.9 | I m m a | 20.299; 23.746; 12.814 90; 90; 90 | 6176.6 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Ca represents an unknown distribution across the Ca sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-150, T = 150 C American Mineralogist, 2004, 89, 1033-1042 |
9003491 | CIF | Al2.12 Ca0.971 O24 Si9.88 | I m m a | 20.053; 23.838; 12.85 90; 90; 90 | 6142.6 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Ca represents an unknown distribution across the Ca sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-350, T = 350 C American Mineralogist, 2004, 89, 1033-1042 |
9003492 | CIF | Al0.357 Ca0.16 O4 Si1.643 | I m m a | 20.041; 23.814; 12.869 90; 90; 90 | 6141.81 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Ca represents an unknown distribution across the Ca sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-500, T = 500 C American Mineralogist, 2004, 89, 1033-1042 |
9003493 | CIF | Al2.14 Ca0.675 H4.78 O25.44 Si9.86 | I m m a | 20.087; 23.8; 12.805 90; 90; 90 | 6121.69 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Ca represents an unknown distribution across the Ca sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-150-R, T = 150 C American Mineralogist, 2004, 89, 1033-1042 |
9003494 | CIF | Al2.46 H8.448 O29.182 Si9.54 | I m m a | 20.295; 23.843; 12.802 90; 90; 90 | 6194.81 | Zanardi, S.; Cruciani, G.; Alberti, A.; Galli, E. Dehydration and rehydration process in boggsite: an in-situ X-ray single-crystal study Note: Ca represents an unknown distribution across the Ca sites of [Ca.806,Mg.138,Na.041,K.007,Fe.006,Sr.001] Note: Reported occupancies are discrepant with reported formula. Sample: BOG-RT-R, T = 25 C American Mineralogist, 2004, 89, 1033-1042 |
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