Crystallography Open Database

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

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9003395 CIFCr Na O6 Si2C 1 2/c 19.697; 8.98; 5.184
90; 109.7; 90
424.997Thompson, 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 CIFCr Na O6 Si2C 1 2/c 19.65; 8.937; 5.16
90; 109.7; 90
418.963Thompson, 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 CIFCr Na O6 Si2C 1 2/c 19.401; 8.738; 5.045
90; 108.7; 90
392.549Thompson, 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 CIFAl Li O6 Si2C 1 2/c 19.57; 8.717; 5.033
90; 112.1; 90
389.014Thompson, 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 CIFAl Li O6 Si2C 1 2/c 19.589; 8.766; 5.061
90; 111.7; 90
395.265Thompson, 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 CIFAl Li O6 Si2C 1 2/c 19.572; 8.715; 5.032
90; 112.1; 90
388.928Thompson, 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 CIFAl Li O6 Si2C 1 2/c 19.503; 8.655; 4.997
90; 112.1; 90
380.799Thompson, 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 CIFFe Li O6 Si2C 1 2/c 19.695; 8.919; 5.149
90; 110.9; 90
415.938Thompson, 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 CIFGa Li O6 Si2C 1 2/c 19.601; 8.839; 5.103
90; 110.7; 90
405.101Thompson, 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 CIFLi O6 Si2 VC 1 2/c 19.648; 8.898; 5.137
90; 110.5; 90
413.073Thompson, 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 CIFLi O6 Sc Si2C 1 2/c 19.838; 9.092; 5.249
90; 110.1; 90
440.912Thompson, 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 CIFAl Na O6 Si2C 1 2/c 19.527; 8.81; 5.087
90; 110; 90
401.217Thompson, 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 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
9003408 CIFFe Na O6 Si2C 1 2/c 19.737; 9.009; 5.201
90; 109.9; 90
428.992Thompson, 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 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
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
9003412 CIFGa Na O6 Si2C 1 2/c 19.64; 8.928; 5.155
90; 109.7; 90
417.702Thompson, 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 CIFIn Na O6 Si2C 1 2/c 19.967; 9.241; 5.335
90; 109.4; 90
463.481Thompson, 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 CIFCa Ni O6 Si2C 1 2/c 19.724; 9.043; 5.221
90; 108.5; 90
435.379Thompson, 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 CIFCa Co O6 Si2C 1 2/c 19.785; 9.1; 5.254
90; 108.5; 90
443.659Thompson, 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 CIFCa Fe O6 Si2C 1 2/c 19.828; 9.142; 5.278
90; 108.4; 90
449.972Thompson, 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 CIFCa Mn O6 Si2C 1 2/c 19.94; 9.248; 5.339
90; 108.3; 90
465.967Thompson, 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 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
9003419 CIFMg O3 SiP 1 21/c 16.928; 6; 3.464
90; 109.47; 90
135.758Thompson, 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 CIFMg O3 SiP 1 21/c 17.559; 6.928; 4
90; 105.3; 90
202.051Thompson, 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 CIFMg O3 SiP 1 21/c 19.725; 8.872; 5.122
90; 108.9; 90
418.101Thompson, 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 CIFMg O3 SiP 1 21/c 19.764; 8.953; 5.169
90; 108.8; 90
427.752Thompson, 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 CIFAl Li O6 Si2P 1 21/c 19.402; 8.587; 4.958
90; 110.2; 90
375.664Thompson, 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 CIFAl Li O6 Si2P 1 21/c 19.292; 8.459; 4.884
90; 109.6; 90
361.644Thompson, 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 CIFMg O3 SiP b c a14.58; 6.928; 4
90; 90; 90
404.041Thompson, 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 CIFMg O3 SiP b c a14.074; 6.928; 4
90; 90; 90
390.019Thompson, 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 CIFMg O3 SiP b c a18.363; 8.867; 5.119
90; 90; 90
833.5Thompson, 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 CIFMg O3 SiP b c a18.535; 9.024; 5.21
90; 90; 90
871.424Thompson, 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 CIFMg O3 SiP b c a18.363; 8.864; 5.118
90; 90; 90
833.055Thompson, 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 CIFMg O3 SiP b c a18.027; 8.683; 5.013
90; 90; 90
784.677Thompson, 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 CIFMg O3 SiP b c n7.037; 6.928; 4
90; 90; 90
195.009Thompson, 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 CIFMg O3 SiP b c n9.268; 9.102; 5.255
90; 90; 90
443.298Thompson, 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 CIFMg O3 SiP b c n9.199; 9.026; 5.211
90; 90; 90
432.67Thompson, 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 CIFMg O3 SiP b c n9.154; 8.981; 5.185
90; 90; 90
426.27Thompson, 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 CIFMg O3 SiP 21 c n6.532; 6; 3.464
90; 90; 90
135.761Thompson, 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 CIFMg O3 SiP 21 c n9.127; 8.877; 5.125
90; 90; 90
415.229Thompson, 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 CIFMg O3 SiP 21 c n9.002; 8.698; 5.022
90; 90; 90
393.22Thompson, 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 CIFCa4.32 F Mn0.68 O12 P3P 63/m9.3429; 9.3429; 6.811
90; 90; 120
514.879Hughes, 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 CIFAl1.96 Ba0.94 H8 O13.54 Si3.04P -4 21 m9.5909; 9.5909; 6.5339
90; 90; 90
601.023Gatta, 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 CIFAl1.96 Ba0.91 H8 O13.32 Si3.04P -4 21 m9.5909; 9.5909; 6.5339
90; 90; 90
601.023Gatta, 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 CIFAl1.96 Ba0.88 H8 O13.32 Si3.04P -4 21 m9.4669; 9.4669; 6.4765
90; 90; 90
580.438Gatta, 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 CIFAl1.96 Ba0.89 H7.68 O13.32 Si3.04P -4 21 m9.3466; 9.3466; 6.42705
90; 90; 90
561.46Gatta, 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 CIFH2 Mg6 Na2 O24 Si8P 1 21/m 19.689; 17.938; 5.268
90; 102.5; 90
893.882Iezzi, 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 CIFAl1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72C 1 2/m 15.337; 9.24; 10.237
90; 100.02; 90
497.126Comodi, 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 CIFAl1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72C 1 2/m 15.318; 9.21; 10.1
90; 100.12; 90
486.989Comodi, 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 CIFAl1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72C 1 2/m 15.291; 9.16; 9.9
90; 100.3; 90
472.077Comodi, 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 CIFAl1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72C 1 2/m 15.271; 9.13; 9.78
90; 100.3; 90
463.07Comodi, 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 CIFAl1.28 Ba0.03 F0.18 Fe0.82 H1.72 K0.91 Mg2.18 Na0.02 O11.82 Si2.72C 1 2/m 15.256; 9.105; 9.71
90; 100.4; 90
457.047Comodi, 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 CIFAs0.975 S3 Sb1.025P 1 21/a 111.949; 9.028; 10.13
90; 116.15; 90
980.926Kyono, A.; Kimata, M.
Structural reinvestigation of getchellite As0.98Sb1.02S3.00
American Mineralogist, 2004, 89, 696-700
9003450 CIFB Ca H O5 SiP 1 21/c 14.85; 7.627; 9.659
90; 90.255; 90
357.292Perchiazzi, 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 CIFB1.25 Ca H1.25 O5 Si0.75P 1 21/c 14.8014; 7.578; 9.5419
90; 90.434; 90
347.172Perchiazzi, 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 CIFB1.25 Ca H1.25 O5 Si0.75P 1 21/c 14.8005; 7.5788; 9.5432
90; 90.437; 90
347.191Perchiazzi, 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 CIFB1.25 Ca H1.25 O5 Si0.75P 1 21/c 14.7967; 7.5711; 9.5321
90; 90.427; 90
346.161Perchiazzi, 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 CIFB1.25 Ca H1.25 O5 Si0.75P 1 21/c 14.7892; 7.5644; 9.5362
90; 90.476; 90
345.46Perchiazzi, 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 CIFB1.25 Ca H1.25 O5 Si0.75P 1 21/c 14.80042; 7.57864; 9.5426
90; 90.435; 90
347.156Perchiazzi, 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 CIFMg O3 SiP b n m4.778; 4.9298; 6.899
90; 90; 90
162.503Dobson, D. P.; Jacobsen, S. D.
The flux growth of magnesium silicate perovskite single crystals
American Mineralogist, 2004, 89, 807-811
9003457 CIFAl0.1 Ca0.06 F0.47 Fe2.63 H1.51 K0.125 Li1.66 Mg1.35 Mn0.13 Na1.376 O23.51 Si8 Ti0.06 Zn0.31C 1 2/m 19.535; 17.876; 5.294
90; 102.54; 90
880.824Oberti, 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 CIFAl0.1 Ca0.11 F0.7 Fe2.06 H1.3 K0.232 Li1.35 Mg1.47 Mn0.12 Na2.411 O23.3 Si8 Ti0.12 Zn0.4C 1 2/m 19.712; 17.851; 5.297
90; 103.63; 90
892.473Oberti, 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 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
9003463 CIFBi0.064 S3 Sb1.936P n m a11.3122; 3.8428; 11.221
90; 90; 90
487.783Kyono, 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 CIFBi0.364 S3 Sb1.636P n m a11.274; 3.8739; 11.16
90; 90; 90
487.406Kyono, 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 CIFBi0.516 S3 Sb1.484P n m a11.318; 3.883; 11.226
90; 90; 90
493.358Kyono, 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 CIFBi0.536 S3 Sb1.464P n m a11.309; 3.871; 11.1876
90; 90; 90
489.761Kyono, 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 CIFBi0.573 S3 Sb1.427P n m a11.318; 3.8872; 11.228
90; 90; 90
493.98Kyono, 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 CIFBi1.09 S3 Sb0.91P n m a11.256; 3.8966; 11.205
90; 90; 90
491.453Kyono, 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 CIFBi1.612 S3 Sb0.388P n m a11.336; 3.9562; 11.186
90; 90; 90
501.664Kyono, 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 CIFBi1.638 S3 Sb0.362P n m a11.31; 3.9526; 11.119
90; 90; 90
497.063Kyono, 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 CIFBi1.68 S3 Sb0.32P n m a11.318; 3.9547; 11.1631
90; 90; 90
499.652Kyono, 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 CIFBi2 S3P n m a11.316; 3.9709; 11.178
90; 90; 90
502.28Kyono, 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 CIFBi2 S3P n m a11.345; 3.994; 11.193
90; 90; 90
507.176Kyono, 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 CIFBi2 S3P n m a11.354; 3.9911; 11.188
90; 90; 90
506.984Kyono, 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 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
9003477 CIFH6.8 O18 Se2 Sr U3C 1 2/m 117.014; 7.0637; 7.1084
90; 100.544; 90
839.875Almond, 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 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
9003479 CIFAl2 Mg O4F d -3 m :28.0834; 8.0834; 8.0834
90; 90; 90
528.18Meducin, 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 CIFAl2 Mg O4F d -3 m :28.0727; 8.0727; 8.0727
90; 90; 90
526.086Meducin, 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 CIFAl2 Mg O4F d -3 m :28.0874; 8.0874; 8.0874
90; 90; 90
528.965Meducin, 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 CIFAl2 Mg O4F d -3 m :28.1104; 8.1104; 8.1104
90; 90; 90
533.491Meducin, 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 CIFAl2 Mg O4F d -3 m :28.1274; 8.1274; 8.1274
90; 90; 90
536.852Meducin, 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 CIFAl2 Mg O4F d -3 m :28.135; 8.135; 8.135
90; 90; 90
538.36Meducin, 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 CIFAl2 Mg O4F d -3 m :28.1452; 8.1452; 8.1452
90; 90; 90
540.387Meducin, 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 CIFAl2 Mg O4F d -3 m :28.1171; 8.1171; 8.1171
90; 90; 90
534.814Meducin, 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 CIFAl2 Mg O4F d -3 m :28.105; 8.105; 8.105
90; 90; 90
532.426Meducin, 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 CIFAl2 Mg O4F d -3 m :28.08; 8.08; 8.08
90; 90; 90
527.514Meducin, 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 CIFAl2.42 H8.448 O30.36 Si9.58I m m a20.291; 23.84; 12.807
90; 90; 90
6195.23Zanardi, 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 CIFAl2.1 Ca0.67 H4.78 O25.31 Si9.9I m m a20.299; 23.746; 12.814
90; 90; 90
6176.6Zanardi, 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 CIFAl2.12 Ca0.971 O24 Si9.88I m m a20.053; 23.838; 12.85
90; 90; 90
6142.6Zanardi, 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 CIFAl0.357 Ca0.16 O4 Si1.643I m m a20.041; 23.814; 12.869
90; 90; 90
6141.81Zanardi, 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 CIFAl2.14 Ca0.675 H4.78 O25.44 Si9.86I m m a20.087; 23.8; 12.805
90; 90; 90
6121.69Zanardi, 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 CIFAl2.46 H8.448 O29.182 Si9.54I m m a20.295; 23.843; 12.802
90; 90; 90
6194.81Zanardi, 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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