Crystallography Open Database

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Searching journal of publication like 'European Journal of Mineralogy (1,1989-)'

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COD ID Up arrow Links Formula Up arrow Space group Up arrow Cell parameters Cell volume Blue up arrow Bibliography
9016237 CIFCo0.008 Cu0.006 Fe0.316 Ir0.202 Ni0.421 Os0.003 Pt0.032 Rh0.006 Ru0.004P 63/m m c2.6939; 2.6939; 4.2732
90; 90; 120
26.856McDonald, A. M.; Proenza, J. A.; Zaccarini, F.; Rudashevsky, N. S.; Cabri, L. J.; Stanley, C. J.; Rudashevsky, V. N.; Melgarejo, J. C.; Lewis, J. F.; Longo, F.; Bakker, R. J.
Garutiite, (Ni,Fe,Ir), a new hexagonal polymorph of native Ni from Loma Peguera, Dominican Republic
European Journal of Mineralogy, 2010, 22, 293-304
9014404 CIFFe Si2P 4/m m m2.696; 2.696; 5.147
90; 90; 90
37.411Li, G.; Bai, W.; Shi, N.; Fang, Q.; Xiong, M.; Yang, J.; Ma, Z.; Rong, H.
Linzhiite, FeSi2, a redefined and revalidated new mineral species from Luobusha, Tibet, China
European Journal of Mineralogy, 2012, 24, 1047-1052
9005699 CIFCa1.59 Mn0.167 O2.187P -32.845; 2.845; 7.485
90; 90; 120
52.467Ertl, A.; Pertlik, F.; Prem, M.; Post, J. E.; Kim, S. J.; Brandstatter, F.; Schuster, R.
Rancieite crystals from Friesach, Carinthia, Austria Note: Birnessite group
European Journal of Mineralogy, 2005, 17, 163-172
9005450 CIFCa0.06 La0.19 Na0.75 Nb0.5 O3 Ti0.5P m -3 m3.909; 3.909; 3.909
90; 90; 90
59.731Krivovichev, S. V.; Chakhmouradian, A. R.; Mitchell, R. H.; Filatov, S. K.; Chukanov, N. V.
Crystal structure of isolueshite and its synthetic compositional analogue Sample: isolueshite
European Journal of Mineralogy, 2000, 12, 597-607
9015340 CIFCr H O2P 21 n m4.8623; 4.2972; 2.9567
90; 90; 90
61.778Jahn, S.; Wunder, B.; Koch-Muller M; Tarrieu, L.; Pohle, M.; Watenphul, A.; Taran, M. N.
Pressure-induced hydrogen bond symmetrisation in guyanaite, B-CrOOH: evidence from spectroscopy and ab initio simulations Sample: Run LT9
European Journal of Mineralogy, 2012, 24, 839-850
9015967 CIFCr H2 O2P n n m4.8623; 4.2972; 2.9567
90; 90; 90
61.778Jahn, S.; Wunder, B.; Koch-Muller M; Tarrieu, L.; Pohle, M.; Watenphul, A.; Taran, M. N.
Pressure-induced hydrogen bond symmetrisation in guyanaite, B-CrOOH: evidence from spectroscopy and ab initio simulations Sample: Run LT9
European Journal of Mineralogy, 2012, 24, 839-850
9014615 CIFCr H2 O2P n n m4.8691; 4.3184; 2.9594
90; 90; 90
62.226Jahn, S.; Wunder, B.; Koch-Muller M; Tarrieu, L.; Pohle, M.; Watenphul, A.; Taran, M. N.
Pressure-induced hydrogen bond symmetrisation in guyanaite, B-CrOOH: evidence from spectroscopy and ab initio simulations Sample: Run #630
European Journal of Mineralogy, 2012, 24, 839-850
9005513 CIFMg OF m -3 m4.2113; 4.2113; 4.2113
90; 90; 90
74.688Boiocchi, M.; Caucia, F.; Merli, M.; Prella, D.; Ungaretti, L.
Crystal-chemical reasons for the immiscibility of periclase and wustite under lithospheric P,T conditions Sample: Per.synt
European Journal of Mineralogy, 2001, 13, 871-881
9005516 CIFFe0.01 Mg0.99 OF m -3 m4.212; 4.212; 4.212
90; 90; 90
74.725Boiocchi, M.; Caucia, F.; Merli, M.; Prella, D.; Ungaretti, L.
Crystal-chemical reasons for the immiscibility of periclase and wustite under lithospheric P,T conditions Sample: after heating to 1100 deg C
European Journal of Mineralogy, 2001, 13, 871-881
9005514 CIFFe0.026 Mg0.974 OF m -3 m4.2154; 4.2154; 4.2154
90; 90; 90
74.906Boiocchi, M.; Caucia, F.; Merli, M.; Prella, D.; Ungaretti, L.
Crystal-chemical reasons for the immiscibility of periclase and wustite under lithospheric P,T conditions Sample: Per.4041
European Journal of Mineralogy, 2001, 13, 871-881
9005515 CIFFe0.042 Mg0.958 OF m -3 m4.2178; 4.2178; 4.2178
90; 90; 90
75.034Boiocchi, M.; Caucia, F.; Merli, M.; Prella, D.; Ungaretti, L.
Crystal-chemical reasons for the immiscibility of periclase and wustite under lithospheric P,T conditions Sample: Per.3363
European Journal of Mineralogy, 2001, 13, 871-881
9005550 CIFCu2.001 SP 63/m m c4.033; 4.033; 6.739
90; 90; 120
94.925Will, G.; Hinze, E.; Abdelrahman, A. R. M.
Crystal structure analysis and refinement of digenite, Cu1.8S, in the temperature range 20 to 500 C under controlled sulfur partial pressure Sample: T = 300 C, sometimes called high-chalcocite
European Journal of Mineralogy, 2002, 14, 591-598
9005017 CIFO2 SiP 32 2 14.9137; 4.9137; 5.4047
90; 90; 120
113.011Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 298 K
European Journal of Mineralogy, 1990, 2, 63-77
9005018 CIFO2 SiP 32 2 14.9209; 4.9209; 5.4091
90; 90; 120
113.434Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 398 K
European Journal of Mineralogy, 1990, 2, 63-77
9005019 CIFO2 SiP 32 2 14.9297; 4.9297; 5.4151
90; 90; 120
113.967Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 498 K
European Journal of Mineralogy, 1990, 2, 63-77
9005020 CIFO2 SiP 32 2 14.9384; 4.9384; 5.4213
90; 90; 120
114.5Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 597 K
European Journal of Mineralogy, 1990, 2, 63-77
9005021 CIFO2 SiP 32 2 14.9509; 4.9509; 5.4285
90; 90; 120
115.234Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 697 K
European Journal of Mineralogy, 1990, 2, 63-77
9005022 CIFO2 SiP 32 2 14.9628; 4.9628; 5.436
90; 90; 120
115.948Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 773 K
European Journal of Mineralogy, 1990, 2, 63-77
9005023 CIFO2 SiP 32 2 14.9728; 4.9728; 5.4425
90; 90; 120
116.555Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 813 K
European Journal of Mineralogy, 1990, 2, 63-77
9005024 CIFO2 SiP 32 2 14.9841; 4.9841; 5.45
90; 90; 120
117.247Kihara, K.
An X-ray study of the temperature dependence of the quartz structure Sample: at T = 838 K
European Journal of Mineralogy, 1990, 2, 63-77

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