Crystallography Open Database

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COD ID	Links	Formula	Space group	Cell parameters	Cell volume	Bibliography
9014067	CIF	Cr2 O3	R -3 c :H	4.629; 4.629; 12.88 90; 90; 120	239.013	Kantor, A.; Kantor, I.; Merlini, M.; Glazyrin, K.; Prescher, C.; Hanfland, M.; Dubrovinsky, L. High-pressure structural studies of eskolaite by means of single-crystal X-ray diffraction Note: P = 63.9 GPa American Mineralogist, 2012, 97, 1764-1770
9014068	CIF	Al0.03 Ba0.6 Fe0.98 H0.4 Mg0.02 O11.4 Si0.86 V5.305 Zn0.11	P -3 m 1	5.75; 5.75; 14.459 90; 90; 120	414.004	Bartholomew, P. R.; Mancini, F.; Harlow, G. E.; Deifel, N.; Cahill, C.; Bernhardt, H. J. Greenwoodite, a new nesosilicate from British Columbia with a Ba-VOH coupled substitution and tetrahedral Fe: description and structure The Canadian Mineralogist, 2012, 50, 1233-1242
9014069	CIF	Al1.33 Fe0.21 Mg0.16 O6 Si0.91	P -3 1 m	4.7621; 4.7621; 4.2964 90; 90; 120	84.379	Boffa Ballaran, T.; Frost, D. J.; Miyajima, N.; Heidelbach, F. The structure of a super-aluminous version of the dense hydrous-magnesium silicate phase D American Mineralogist, 2010, 95, 1113-1116
9014071	CIF	C0.097 H3.224 Cr0.19 Mg0.81 O2.903	P 63/m m c	3.09646; 3.09646; 15.627 90; 90; 120	129.759	Mills, S. J.; Whitfield, P. S.; Wilson, S. A.; Woodhouse, J. N.; Dipple, G. M.; Raudsepp, M.; Francis, C. A. The crystal structure of stichtite, re-examination of barbertonite, and the nature of polytypism in MgCr hydrotalcites Note: Sample 92459, 2H1 polytype of stichtite American Mineralogist, 2011, 96, 179-187
9014073	CIF	Ca9 F0.784 H1.2 O17.216 Si4	P 21/b 1 1	5.0672; 11.3545; 15.3941 100.587; 90; 90	870.63	Galuskin, E. V.; Lazic, B.; Armbruster, T.; Galuskina, I. O.; Pertsev, N. N.; Gazeev, V. M.; Wlodyka, R.; Dulski, M.; Dzierzanowski, P.; Zadov, A. E.; Dubrovinsky, L. S. Edgrewite Ca9(SiO4)4F2-hydroxyledgrewite Ca9(SiO4)4(OH)2, a new series of calcium humite-group minerals from altered xenoliths in the ignimbrite of Upper Chegem caldera, Northern Caucasus, Kabardino-Balkaria, Russia American Mineralogist, 2012, 97, 1998-2006

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