Crystallography Open Database

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Searching space group like 'P 1 21/c 1'

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9013470 CIFHf O2P 1 21/c 15.1156; 5.1722; 5.2948
90; 99.18; 90		138.3Ruh, R.; Corfield, P. W. R.
Crystal structure of monoclinic hafnia and comparison with monoclinic zirconia Locality: synthetic
Journal of the American Ceramic Society, 1970, 53, 126-129
9013617 CIFFe Ge2 Li O6P 1 21/c 19.893; 8.836; 5.379
90; 108.83; 90		445.038Nestola, F.; Redhammer, G. J.; Pamato, M. G.; Secco, L.; Dal Negro, A.
High-pressure phase transformation in LiFeGe2O6 pyroxene Note: P = 0.00 GPa
American Mineralogist, 2009, 94, 616-621
9013661 CIFH10 Mg Na2 O13 S2P 1 21/c 15.769; 23.951; 8.046
90; 95.425; 90		1106.76Leduc, E. M. S.; Peterson, R. C.; Wang, R.
The crystal structure and hydrogen bonding of synthetic konyaite, Na2Mg(SO4)2*5H2O Locality: synthetic
American Mineralogist, 2009, 94, 1005-1011
9013706 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.749; 8.937; 5.246
90; 108.49; 90		433.473Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 0.0001 GPa
American Mineralogist, 2010, 95, 300-311
9013707 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.722; 8.941; 5.247
90; 108.5; 90		432.523Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 0.047 GPa
American Mineralogist, 2010, 95, 300-311
9013708 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.701; 8.887; 5.226
90; 108.38; 90		427.564Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 0.984 GPa
American Mineralogist, 2010, 95, 300-311
9013709 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.659; 8.877; 5.218
90; 108.09; 90		425.291Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 1.794 GPa
American Mineralogist, 2010, 95, 300-311
9013710 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.621; 8.827; 5.199
90; 107.82; 90		420.34Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 3.167 GPa
American Mineralogist, 2010, 95, 300-311
9013711 CIFAl0.02 Ca0.121 Fe1.008 Mg0.871 O6 Si1.98P 1 21/c 19.622; 8.861; 5.181
90; 107.92; 90		420.305Alvaro, M.; Nestola, F.; Ballaran, T. B.; Camara, F.; Domeneghetti, M. C.; Tazzoli, V.
High-pressure phase transition of a natural pigeonite Note: P = 3.172 GPa
American Mineralogist, 2010, 95, 300-311
9013794 CIFCa3.58 Ce1.1 F0.9 H2.738 Na0.24 Nb0.04 O17.8 Si4 Ti0.96 Zr0.08P 1 21/c 17.398; 5.595; 18.662
90; 101.37; 90		757.294Bellezza, M.; Merlino, S.; Perchiazzi, N.
Mosandrite: Structural and crystal-chemical relationships with rinkite Norway
The Canadian Mineralogist, 2009, 47, 897-908
9013856 CIFGa Li O6 Si2P 1 21/c 19.5092; 8.5684; 5.2345
90; 109.86; 90		401.134Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 100 K
European Journal of Mineralogy, 2009, 21, 599-614
9013857 CIFGa Li O6 Si2P 1 21/c 19.5112; 8.5703; 5.2354
90; 109.88; 90		401.326Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 125 K
European Journal of Mineralogy, 2009, 21, 599-614
9013858 CIFGa Li O6 Si2P 1 21/c 19.5134; 8.5705; 5.2372
90; 109.91; 90		401.49Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 150 K
European Journal of Mineralogy, 2009, 21, 599-614
9013859 CIFGa Li O6 Si2P 1 21/c 19.5161; 8.5708; 5.2397
90; 109.92; 90		401.784Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 175 K
European Journal of Mineralogy, 2009, 21, 599-614
9013860 CIFGa Li O6 Si2P 1 21/c 19.5189; 8.5722; 5.2428
90; 109.93; 90		402.18Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 200 K
European Journal of Mineralogy, 2009, 21, 599-614
9013861 CIFGa Li O6 Si2P 1 21/c 19.5193; 8.5713; 5.2466
90; 109.99; 90		402.294Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 225 K
European Journal of Mineralogy, 2009, 21, 599-614
9013862 CIFGa Li O6 Si2P 1 21/c 19.5277; 8.5722; 5.2512
90; 109.99; 90		403.044Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 250 K
European Journal of Mineralogy, 2009, 21, 599-614
9013863 CIFGa Li O6 Si2P 1 21/c 19.5267; 8.5688; 5.2553
90; 110.06; 90		402.977Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 265 K
European Journal of Mineralogy, 2009, 21, 599-614
9013864 CIFGa Li O6 Si2P 1 21/c 19.5405; 8.563; 5.2669
90; 110.15; 90		403.945Camara, F.; Nestola, F.; Angel, R. J.; Ohashi, H.
Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Note: T = 280 K
European Journal of Mineralogy, 2009, 21, 599-614
9013917 CIFAl2 Ca O4P 1 21/c 17.97187; 8.62844; 10.26276
90; 94.801; 90		703.445Lazic, B.; Kahlenberg, V.; Konzett, J.
Structural studies on a stuffed framework high pressure polymorph of CaAl2O4
Zeitschrift fur Kristallographie, 2007, 222, 690-695

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All data in the COD and the database itself are dedicated to the public domain and licensed under the CC0 License . Users of the data should acknowledge the original authors of the structural data.