Crystallography Open Database

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Searching journal of publication like 'Physics and Chemistry of Minerals' volume of publication is 16

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9005867 CIFK2 Mn2 O12 S3P 21 310.1073; 10.1073; 10.1073
90; 90; 90
1032.54Oelkrug, H.; Bruckel, T.; Hohlwein, D.; Hoser, A.; Prandl, W.
The magnetic structure of the langbeinite K2Mn2(SO4)3
Physics and Chemistry of Minerals, 1988, 16, 246-249
9005868 CIFK2 Mn2 O12 S3P 21 21 2110.0443; 10.0735; 10.0036
90; 90; 90
1012.18Oelkrug, H.; Bruckel, T.; Hohlwein, D.; Hoser, A.; Prandl, W.
The magnetic structure of the langbeinite K2Mn2(SO4)3 Sample at T = 4.2 K Note, there is something wrong with this dataset.
Physics and Chemistry of Minerals, 1988, 16, 246-249
9005869 CIFMg O3 SiP b n m4.7786; 4.9293; 6.9003
90; 90; 90
162.538Ross, N. L.; Hazen, R. M.
Single crystal X-ray diffraction study of MgSiO3 perovskite from 77 to 400 K Sample: Crystal 1
Physics and Chemistry of Minerals, 1989, 16, 415-420
9005870 CIFMg O3 SiP b n m4.7747; 4.9319; 6.8987
90; 90; 90
162.453Ross, N. L.; Hazen, R. M.
Single crystal X-ray diffraction study of MgSiO3 perovskite from 77 to 400 K Sample: Crystal 2
Physics and Chemistry of Minerals, 1989, 16, 415-420
9005871 CIFCa Fe3 H O9 Si2P 1 21/a 113.0387; 8.8204; 5.864
90; 90.266; 90
674.391Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 295 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005872 CIFCa Fe3 H O9 Si2P 1 21/a 113.0398; 8.8217; 5.8644
90; 90.244; 90
674.595Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 320 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005873 CIFCa Fe3 H O9 Si2P 1 21/a 113.0466; 8.8268; 5.8647
90; 90.124; 90
675.376Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 340 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005874 CIFCa Fe3 H O9 Si2P 1 21/a 113.0497; 8.8291; 5.8652
90; 90.029; 90
675.771Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 360 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005875 CIFCa Fe3 H O9 Si2P n a m13.0533; 8.8345; 5.8674
90; 90; 90
676.625Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 380 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005876 CIFCa Fe3 H O9 Si2P n a m13.0531; 8.8344; 5.8692
90; 90; 90
676.814Ghose, S.; Tsukimura, K.; Hatch, D. M.
Phase transitions in ilvaite, a mixed-valence iron silicate II. A single-crystal X-ray diffraction study and Landau theory of the monoclinic to orthorhombic phase transition induced by charge delocalization Sample: T = 400 K
Physics and Chemistry of Minerals, 1989, 16, 483-496
9005877 CIFCd2 K2 O12 S3P 21 310.2643; 10.2643; 10.2643
90; 90; 90
1081.4Percival, M. J. L.; Schmahl, W. W.; Salje, E.
Structure of cobalt doped K2Cd2(SO4)3 langbeinite at three temperatures above the P2_13-P2_12_12_1 phase transition, and a new trigger mechanism for the ferroelastic transformation Sample: T = 440 K
Physics and Chemistry of Minerals, 1989, 16, 569-575
9005878 CIFCd2 K2 O12 S3P 21 310.285; 10.285; 10.285
90; 90; 90
1087.96Percival, M. J. L.; Schmahl, W. W.; Salje, E.
Structure of cobalt doped K2Cd2(SO4)3 langbeinite at three temperatures above the P2_13-P2_12_12_1 phase transition, and a new trigger mechanism for the ferroelastic transformation Sample: T = 540 K
Physics and Chemistry of Minerals, 1989, 16, 569-575
9005879 CIFCd2 K2 O12 S3P 21 310.3043; 10.3043; 10.3043
90; 90; 90
1094.1Percival, M. J. L.; Schmahl, W. W.; Salje, E.
Structure of cobalt doped K2Cd2(SO4)3 langbeinite at three temperatures above the P2_13-P2_12_12_1 phase transition, and a new trigger mechanism for the ferroelastic transformation Sample: T = 640 K
Physics and Chemistry of Minerals, 1989, 16, 569-575
9005880 CIFMn O3 TiP b n m5.1048; 5.3046; 7.418
90; 90; 90
200.871Ross, N. L.; Ko, J.; Prewitt, C. T.
A new phase transition in MnTiO3: LiNbO3-perovskite structure Sample: P = 4.5 GPa
Physics and Chemistry of Minerals, 1989, 16, 621-629
9005881 CIFCd Ge O3P b n m5.2114; 5.2608; 7.4263
90; 90; 90
203.6Susaki, J.
CdGeO3-phase transformations at high pressure and temperature and structural refinement of the perovskite polymorph
Physics and Chemistry of Minerals, 1989, 16, 634-641
9005882 CIFFe0.992 Na0.978 O6 Si1.96C 1 2/c 19.68; 8.83; 5.3
90; 107.3; 90
432.52Ballet, O.; Coey, J. M. D.; Fillion, G.; Ghose, A.; Hewat, A. W.; Regnard, J. R.
Magnetic order in acmite; NaFeSi2O6 Sample: T = 14 K
Physics and Chemistry of Minerals, 1989, 16, 672-677

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