Crystallography Open Database
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Result: there are 88 entries in the selection
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Searching journal of publication like 'American Mineralogist' volume of publication is 81
COD ID | Links | Formula | Space group | Cell parameters | Cell volume | Bibliography |
---|---|---|---|---|---|---|
1538122 | CIF | Al3.06 Ca2.45 F1.46 Fe0.43 H0.54 K0.04 Mg3.79 Mn0.06 Na0.41 O22.54 Si5.72 | C 1 2/m 1 | 9.816; 17.899; 5.297 90; 105.35; 90 | 897.465 | Hawthorne, F.C.; Ungaretti, L.; Oberti, R.; Grice, J.D. A new hyper-calcic amphibole with Ca at the A site: Fluor-cannilloite from Pargas, Finland American Mineralogist, 1996, 81, 995-1002 |
1538124 | CIF | Al2.36 Ca2.16 F1.54 Fe0.18 H0.46 K0.4 Mg4.32 Na0.44 O22.46 Si6.14 | C 1 2/m 1 | 9.889; 17.978; 5.298 90; 105.41; 90 | 908.04 | Hawthorne, F.C.; Oberti, R.; Ungaretti, L.; Grice, J.D. A new hyper-calcic amphibole with Ca at the A site: Fluor-cannilloite from Pargas, Finland American Mineralogist, 1996, 81, 995-1002 |
9001713 | CIF | H8 Mn2 O10 Si2 Sr | P 21 c n | 6.247; 9.034; 13.401 90; 90; 90 | 756.291 | Libowitzky, E.; Armbruster, T. Lawsonite-type phase transitions in hennomartinite, SrMn2[Si2O7](OH)2.H2O T = 22 C American Mineralogist, 1996, 81, 9-18 |
9001714 | CIF | H4 Mn2 O10 Si2 Sr | C m c m | 6.255; 9.067; 13.431 90; 90; 90 | 761.727 | Libowitzky, E.; Armbruster, T. Lawsonite-type phase transitions in hennomartinite, SrMn2[Si2O7](OH)2.H2O T = 245 C American Mineralogist, 1996, 81, 9-18 |
9001715 | CIF | Al2 Co3 O12 Si3 | I a -3 d | 11.4597; 11.4597; 11.4597 90; 90; 90 | 1504.94 | Ross, C. R.; Keppler, H.; Canil, D.; O'Neill H St C Structure and crystal-field spectra of Co3Al2(SiO4)3 and (Mg,Ni)3Al2(SiO4)3 garnet Co3Al2(SiO4)3 American Mineralogist, 1996, 81, 61-66 |
9001716 | CIF | Al2 Mg2.55 Ni0.45 O12 Si3 | I a -3 d | 11.4717; 11.4717; 11.4717 90; 90; 90 | 1509.68 | Ross, C. R.; Keppler, H.; Canil, D.; O'Neill H St C Structure and crystal-field spectra of Co3Al2(SiO4)3 and (Mg,Ni)3Al2(SiO4)3 garnet (Mg,Ni)3Al2(SiO4)3 American Mineralogist, 1996, 81, 61-66 |
9001717 | CIF | Mg3 O9 Si2 | C 1 m 1 | 5.323; 9.214; 21.381 90; 90; 90 | 1048.66 | Banfield, J. F.; Bailey, S. W. Formation of regularly interstatified serpentine-chlorite minerals by tetrahedral inversion in long-period serpentine polytypes American Mineralogist, 1996, 81, 79-91 |
9001718 | CIF | Al2.34 Cs0.88 F0.2 Fe0.16 H1.8 K0.06 Li0.14 Mg0.2 O11.8 Rb0.01 Si3.16 | C 1 2/c 1 | 9.076; 5.226; 21.41 90; 99.48; 90 | 1001.63 | Ni, Y.; Hughes, J. M. The crystal structure of nanpingite-2M2, the Cs end-member of muscovite American Mineralogist, 1996, 81, 105-110 |
9001719 | CIF | H6 O14 S Zn4 | P -3 | 8.33; 8.33; 10.54 90; 90; 120 | 633.375 | Groat, L. A. The crystal structure of namuwite, a mineral with Zn in tetrahedral and octahedral coordination, and its relationship to the synthetic basic zinc sulfates Note: U(1,2) for S has been changed to match symmetry constraints. American Mineralogist, 1996, 81, 238-243 |
9001720 | CIF | Cu1.002 H19 O21 S Si Zn6.938 | P -3 | 8.319; 8.319; 7.377 90; 90; 120 | 442.133 | Giester, G.; Rieck, B. Bechererite, (Zn,Cu)6Zn2(OH)13[(S,Si)(O,OH)4]2, a novel mineral species from the Tonopah-Belmont mine, Arizonia Note: U(1,2) changed for Si, S, O1, OH1 to match symmetry constraints. American Mineralogist, 1996, 81, 244-248 |
9001721 | CIF | Li O4 Sc Si | P b n m | 4.8168; 10.4317; 5.965 90; 90; 90 | 299.726 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #0, P = 0.0 GPa American Mineralogist, 1996, 81, 327-334 |
9001722 | CIF | Li O4 Sc Si | P b n m | 4.8189; 10.4373; 5.9695 90; 90; 90 | 300.244 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #1, P = 0.06 GPa American Mineralogist, 1996, 81, 327-334 |
9001723 | CIF | Li O4 Sc Si | P b n m | 4.8198; 10.4378; 5.9699 90; 90; 90 | 300.334 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 0.21 GPa American Mineralogist, 1996, 81, 327-334 |
9001724 | CIF | Li O4 Sc Si | P b n m | 4.819; 10.4333; 5.9672 90; 90; 90 | 300.019 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 0.23 GPa American Mineralogist, 1996, 81, 327-334 |
9001725 | CIF | Li O4 Sc Si | P b n m | 4.804; 10.4117; 5.9533 90; 90; 90 | 297.771 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 0.99 GPa American Mineralogist, 1996, 81, 327-334 |
9001726 | CIF | Li O4 Sc Si | P b n m | 4.7996; 10.3925; 5.9443 90; 90; 90 | 296.501 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #1, P = 1.46 GPa American Mineralogist, 1996, 81, 327-334 |
9001727 | CIF | Li O4 Sc Si | P b n m | 4.7918; 10.3784; 5.9365 90; 90; 90 | 295.229 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 2.17 GPa American Mineralogist, 1996, 81, 327-334 |
9001728 | CIF | Li O4 Sc Si | P b n m | 4.7802; 10.3514; 5.9224 90; 90; 90 | 293.051 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 3.02 GPa American Mineralogist, 1996, 81, 327-334 |
9001729 | CIF | Li O4 Sc Si | P b n m | 4.7717; 10.332; 5.9128 90; 90; 90 | 291.508 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 3.72 GPa American Mineralogist, 1996, 81, 327-334 |
9001730 | CIF | Li O4 Sc Si | P b n m | 4.7611; 10.3072; 5.9006 90; 90; 90 | 289.564 | Hazen, R. M.; Downs, R. T.; Finger, L. W. High-pressure crystal chemistry of LiScSiO4: An olivine with nearly isotropic compression Sample: #2, P = 4.51 GPa American Mineralogist, 1996, 81, 327-334 |
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