Crystallography Open Database

Result: there are 474 entries in the selection

Switch to the old layout of the page

Download all results as: list of COD numbers | list of CIF URLs | data in CSV format | archive of CIF files (ZIP)

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

Left arrow Left arrow First | Left arrow Previous 100 | of 5 | Next 100 Blue right arrow | Last Blue right arrow Blue right arrow | Display 5 20 50 100 200 300 500 1000 entries per page

COD ID Up arrow Links Formula Up arrow Space group Blue up arrow Cell parameters Cell volume Up arrow Bibliography
9003556 CIFH3 Mg5 Na3 O24 Si8C -19.883; 54.082; 5.277
90.045; 103.068; 89.96
2747.47Camara, 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 CIFAl2 H1.42 Mg6 Na0.58 O18 Si4C 15.358; 9.281; 14.574
90; 97.08; 90
719.204Krivovichev, 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 CIFH2 Mg2 Na0.193 O6 Si1.333C 15.358; 9.281; 14.574
90; 97.08; 90
719.204Krivovichev, 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 CIFCa0.15 Mg1.85 O6 Si2C 1 2/c 19.291; 8.679; 4.963
90; 102.22; 90
391.132Nestola, 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 CIFH7.79 O25 Pb3 U6C 1 2/c 128.355; 11.99; 13.998
90; 104.248; 90
4612.6Brugger, 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 CIFMg O3 SiC 1 2/c 17.394; 6; 3.464
90; 117.9; 90
135.814Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 240 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003383 CIFMg O3 SiC 1 2/c 17.565; 6.51; 3.759
90; 115.8; 90
166.67Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 220 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003384 CIFMg O3 SiC 1 2/c 17.608; 6.823; 3.939
90; 113.4; 90
187.654Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 200 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003385 CIFMg O3 SiC 1 2/c 17.526; 6.928; 4
90; 110.8; 90
194.968Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 180 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003386 CIFMg O3 SiC 1 2/c 17.326; 6.823; 3.939
90; 107.7; 90
187.572Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 160 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003387 CIFMg O3 SiC 1 2/c 17.023; 6.51; 3.759
90; 104.1; 90
166.683Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 140 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003388 CIFMg O3 SiC 1 2/c 16.6332; 6; 3.464
90; 100; 90
135.77Thompson, R. M.; Downs, R. T.
Model pyroxenes II: Structural variation as a function of tetrahedral rotation model with O3-O3-O3 angle = 120 and model oxygen radius = 1 Note: Atoms Mg, Si, and O are assigned to atomic positions for convenience
American Mineralogist, 2004, 89, 614-628
9003389 CIFCa Mg O6 Si2C 1 2/c 19.756; 9.067; 5.235
90; 108.7; 90
438.63Thompson, 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 CIFCa Mg O6 Si2C 1 2/c 19.876; 9.17; 5.294
90; 109; 90
453.32Thompson, 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 CIFCa Mg O6 Si2C 1 2/c 19.76; 9.071; 5.237
90; 108.7; 90
439.171Thompson, 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 CIFCa Mg O6 Si2C 1 2/c 19.607; 8.939; 5.161
90; 108.3; 90
420.796Thompson, 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 CIFFe O3 SiC 1 2/c 19.552; 8.844; 5.106
90; 103.8; 90
418.893Thompson, 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 CIFCr Na O6 Si2C 1 2/c 19.653; 8.944; 5.164
90; 109.6; 90
420.008Thompson, 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 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
9003315 CIFAl1.74 Ba0.09 F0.02 Fe0.21 H1.98 K0.91 Mg0.93 Mn1.53 O11.98 Si2.56 Ti0.03C 1 2/m 15.3791; 9.319; 10.2918
90; 100.186; 90
507.774Ishida, 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 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
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
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
9003560 CIFBa0.906 H11.6 K1.708 Mn0.493 Na2.196 O32.986 Si8 Ti4C 1 2/m 114.2147; 13.764; 7.7574
90; 116.653; 90
1356.47Armbruster, T.; Krivovichev, S. V.; Weber, T.; Gnos, E.; Organova, N. N.; Yakovenchuk, V. N.
Origin of diffuse superstructure reflections in labuntsovite-group minerals Sample A2 at T = -160 deg C
American Mineralogist, 2004, 89, 1655-1666
9003561 CIFBa0.906 H11.6 K1.708 Mn0.493 Na2.196 O32.986 Si8 Ti4C 1 2/m 114.2446; 13.7884; 7.7798
90; 116.709; 90
1364.99Armbruster, T.; Krivovichev, S. V.; Weber, T.; Gnos, E.; Organova, N. N.; Yakovenchuk, V. N.
Origin of diffuse superstructure reflections in labuntsovite-group minerals Sample A2 at T = 22 deg C
American Mineralogist, 2004, 89, 1655-1666
9003562 CIFBa0.76 Fe0.46 H11.6 K1.78 Na2.22 O36.92 Si8 Ti4C 1 2/m 114.237; 13.768; 7.767
90; 116.83; 90
1358.56Armbruster, T.; Krivovichev, S. V.; Weber, T.; Gnos, E.; Organova, N. N.; Yakovenchuk, V. N.
Origin of diffuse superstructure reflections in labuntsovite-group minerals Sample B at T = 22 deg C
American Mineralogist, 2004, 89, 1655-1666
9003565 CIFBa2 H24 K4 Mn Na4 O66 Si16 Ti8C 1 2/m 114.2446; 13.7884; 15.5
90; 116.709; 90
2719.53Armbruster, T.; Krivovichev, S. V.; Weber, T.; Gnos, E.; Organova, N. N.; Yakovenchuk, V. N.
Origin of diffuse superstructure reflections in labuntsovite-group minerals Note: Predicted ordered structure
American Mineralogist, 2004, 89, 1655-1666
1533075 CIFCa H5 O6 PC 1 c 16.41; 15.18; 5.86
90; 119.2; 90
497.74Sainz-Diaz, C.I.; Villacampa, A.; Otalora, F.
Crystallographic properties of the calcium phosphate mineral, brushite, by means of first principles calculations
American Mineralogist, 2004, 89, 307-313
9003563 CIFBa H10 K2 Na2 O32 Si8 Ti4C 1 m 114.2446; 13.7884; 7.75
90; 116.709; 90
1359.76Armbruster, T.; Krivovichev, S. V.; Weber, T.; Gnos, E.; Organova, N. N.; Yakovenchuk, V. N.
Origin of diffuse superstructure reflections in labuntsovite-group minerals Note: Predicted ordered structure
American Mineralogist, 2004, 89, 1655-1666
9003354 CIFAl1.956 Ca0.466 H34 K0.24 Na0.69 O31.18 Si10.044C m c 2118.096; 20.473; 7.515
90; 90; 90
2784.15Simoncic, P.; Armbruster, T.
Peculiarity and defect structure of the natural and synthetic zeolite mordenite: A single-crystal X-ray study Sample: natural
American Mineralogist, 2004, 89, 421-431
9003355 CIFAl1.5 H30 Na1.37 O28.86 Si10.5C m c 2118.131; 20.507; 7.5221
90; 90; 90
2796.81Simoncic, P.; Armbruster, T.
Peculiarity and defect structure of the natural and synthetic zeolite mordenite: A single-crystal X-ray study Sample: synthetic
American Mineralogist, 2004, 89, 421-431
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
9003531 CIFAl0.393 Cr1.582 Fe0.34 Mg0.59 Mn0.003 Ni0.004 O4 Si0.002 Ti0.004 V0.004F d -3 m :28.2743; 8.2743; 8.2743
90; 90; 90
566.492Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Tro6f, Provenance is Tropoja massif, Sequence is cumulate
American Mineralogist, 2004, 89, 1367-1373
9003532 CIFAl0.406 Cr1.524 Fe0.396 Mg0.643 Mn0.006 Ni0.002 O4 Ti0.006F d -3 m :28.2991; 8.2991; 8.2991
90; 90; 90
571.601Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shb4b, Provenance is Shebenik massif, Sequence is cumulate
American Mineralogist, 2004, 89, 1367-1373
9003533 CIFAl0.552 Cr1.362 Fe0.481 Mg0.586 Mn0.007 Ni0.004 O4 Ti0.006F d -3 m :28.2915; 8.2915; 8.2915
90; 90; 90
570.032Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Tro4f, Provenance is Tropoja massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003534 CIFAl0.575 Cr1.346 Fe0.429 Mg0.631 Mn0.006 Ni0.002 O4 Ti0.006 V0.004F d -3 m :28.2864; 8.2864; 8.2864
90; 90; 90
568.981Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Tro4j, Provenance is Tropoja massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003535 CIFAl0.364 Cr1.552 Fe0.467 Mg0.597 Mn0.008 O4 Ti0.004 V0.004F d -3 m :28.3133; 8.3133; 8.3133
90; 90; 90
574.54Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: N10a, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003536 CIFAl0.393 Cr1.5 Fe0.469 Mg0.608 Mn0.009 Ni0.002 O4 Ti0.006F d -3 m :28.3091; 8.3091; 8.3091
90; 90; 90
573.67Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: N7g, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003537 CIFAl0.368 Cr1.564 Fe0.424 Mg0.624 Mn0.007 O4 Ti0.002F d -3 m :28.3081; 8.3081; 8.3081
90; 90; 90
573.463Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Thkv1a, Provenance is Thekna, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003538 CIFAl0.387 Cr1.552 Fe0.402 Mg0.632 Mn0.006 O4 Ti0.002 V0.004F d -3 m :28.3033; 8.3033; 8.3033
90; 90; 90
572.469Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Thkv1w, Provenance is Thekna, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003539 CIFAl0.422 Cr1.506 Fe0.367 Mg0.643 Mn0.004 Ni0.004 O4 Ti0.004 V0.002F d -3 m :28.2793; 8.2793; 8.2793
90; 90; 90
567.52Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shb2m, Provenance is Shebenik massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003540 CIFAl0.444 Cr1.5 Fe0.378 Mg0.637 Mn0.006 Ni0.004 O4 Si0.001 Ti0.002 V0.004F d -3 m :28.2902; 8.2902; 8.2902
90; 90; 90
569.764Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shb4f, Provenance is Shebenik massif, Sequence is cumulate
American Mineralogist, 2004, 89, 1367-1373
9003541 CIFAl0.378 Cr1.536 Fe0.394 Mg0.667 Mn0.007 Ni0.004 O4 Si0.001 Ti0.002 V0.002 Zn0.002F d -3 m :28.3057; 8.3057; 8.3057
90; 90; 90
572.966Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Thkv2w, Provenance is Thekna, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003542 CIFAl0.388 Cr1.548 Fe0.4 Mg0.648 Mn0.006 O4 Si0.001 Ti0.002 V0.002F d -3 m :28.3071; 8.3071; 8.3071
90; 90; 90
573.256Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: N2h, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003543 CIFAl0.438 Cr1.474 Fe0.384 Mg0.682 Mn0.006 Ni0.004 O4 Si0.002 Ti0.004 V0.002F d -3 m :28.3006; 8.3006; 8.3006
90; 90; 90
571.911Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shkm1i, Provenance is Shkalla, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003544 CIFAl0.451 Cr1.466 Fe0.414 Mg0.646 Mn0.007 Ni0.004 O4 Ti0.004F d -3 m :28.2982; 8.2982; 8.2982
90; 90; 90
571.415Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shkm3g, Provenance is Shkalla, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003545 CIFAl0.355 Cr1.55 Fe0.369 Mg0.704 Mn0.006 Ni0.004 O4 Si0.001 Ti0.004 V0.002F d -3 m :28.3101; 8.3101; 8.3101
90; 90; 90
573.877Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Ba4c, Provenance is Bater, Bulqiza massif, Sequence is cumulate
American Mineralogist, 2004, 89, 1367-1373
9003546 CIFAl1.238 Cr0.704 Fe0.304 Mg0.734 Mn0.004 Ni0.006 O4 Ti0.006F d -3 m :28.1992; 8.1992; 8.1992
90; 90; 90
551.207Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: N4x, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite
American Mineralogist, 2004, 89, 1367-1373
9003547 CIFAl0.337 Cr1.606 Fe0.326 Mg0.694 Mn0.006 Ni0.004 O4 Ti0.002 V0.002F d -3 m :28.3043; 8.3043; 8.3043
90; 90; 90
572.676Bosi, F.; Andreozzi, G. B.; Ferrini, V.; Lucchesi, S.
Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Ba2y, Provenance is Bater, Bulqiza massif, Sequence is cumulate
American Mineralogist, 2004, 89, 1367-1373
9003112 CIFCl KF m -3 m6.2879; 6.2879; 6.2879
90; 90; 90
248.609Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: msl515031, T = 25 C, P = 0.0 kbar, cell volume = 248.61 ang**3
American Mineralogist, 2004, 89, 204-210
9003113 CIFCl KF m -3 m6.2987; 6.2987; 6.2987
90; 90; 90
249.892Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57689, T = 36 C, P = 0.4 kbar, cell volume = 249.89 ang**3
American Mineralogist, 2004, 89, 204-210
9003114 CIFCl KF m -3 m6.3122; 6.3122; 6.3122
90; 90; 90
251.502Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: msl515032, T = 100 C, P = 0.0 kbar, cell volume = 251.50 ang**3
American Mineralogist, 2004, 89, 204-210
9003115 CIFCl KF m -3 m6.2843; 6.2843; 6.2843
90; 90; 90
248.182Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57797, T = 100 C, P = 1.9 kbar, cell volume = 248.18 ang**3
American Mineralogist, 2004, 89, 204-210
9003116 CIFCl KF m -3 m6.261; 6.261; 6.261
90; 90; 90
245.432Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57761, T = 100 C, P = 3.9 kbar, cell volume = 245.43 ang**3
American Mineralogist, 2004, 89, 204-210
9003117 CIFCl KF m -3 m6.2137; 6.2137; 6.2137
90; 90; 90
239.911Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57749, T = 100 C, P = 8.6 kbar, cell volume = 239.91 ang**3
American Mineralogist, 2004, 89, 204-210
9003118 CIFCl KF m -3 m6.1573; 6.1573; 6.1573
90; 90; 90
233.438Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57701, T = 100 C, P = 15.0 kbar, cell volume = 233.44 ang**3
American Mineralogist, 2004, 89, 204-210
9003119 CIFCl KF m -3 m6.3361; 6.3361; 6.3361
90; 90; 90
254.37Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: msl515033, T = 200 C, P = 0.0 kbar, cell volume = 254.37 ang**3
American Mineralogist, 2004, 89, 204-210
9003120 CIFCl KF m -3 m6.2849; 6.2849; 6.2849
90; 90; 90
248.253Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57793, T = 200 C, P = 3.1 kbar, cell volume = 248.25 ang**3
American Mineralogist, 2004, 89, 204-210
9003121 CIFCl KF m -3 m6.2593; 6.2593; 6.2593
90; 90; 90
245.232Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57765, T = 200 C, P = 5.5 kbar, cell volume = 245.23 ang**3
American Mineralogist, 2004, 89, 204-210
9003122 CIFCl KF m -3 m6.2187; 6.2187; 6.2187
90; 90; 90
240.491Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57745, T = 200 C, P = 10.2 kbar, cell volume = 240.49 ang**3
American Mineralogist, 2004, 89, 204-210
9003123 CIFCl KF m -3 m6.1671; 6.1671; 6.1671
90; 90; 90
234.554Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57705, T = 200 C, P = 15.7 kbar, cell volume = 234.55 ang**3
American Mineralogist, 2004, 89, 204-210
9003124 CIFCl KF m -3 m6.363; 6.363; 6.363
90; 90; 90
257.624Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: msl515034, T = 300 C, P = 0.0 kbar, cell volume = 257.62 ang**3
American Mineralogist, 2004, 89, 204-210
9003125 CIFCl KF m -3 m6.2682; 6.2682; 6.2682
90; 90; 90
246.28Walker, D.; Verma, P. K.; Cranswick, L. M. D.; Jones, R. L.; Clark, S. M.; Buhre, S.
Halite-sylvite thermoelasticity Sample: r57769, T = 300 C, P = 6.7 kbar, cell volume = 246.28 ang**3
American Mineralogist, 2004, 89, 204-210

Left arrow Left arrow First | Left arrow Previous 100 | of 5 | Next 100 Blue right arrow | Last Blue right arrow Blue right arrow | Display 5 20 50 100 200 300 500 1000 entries per page

Back to the search form
Your own data is not in the COD? Deposit it, thanks!