Crystallography Open Database

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Searching journal of publication like 'American Mineralogist' volume of publication is 93

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9010399 CIFCa3 H2 O9 Si2 Zr0.5P n n m5.666; 18.844; 3.728
90; 90; 90
398.039Kadiyski, M.; Armbruster, T.; Galuskin, E. V.; Pertsev, N. N.; Zadov, A. E.; Galuskina, I. O.; Wrzalik, R.; Dzierzanowski, P.; Kislov, E. V.
The modular structure of dovyrenite, Ca6Zr[Si2O7]2(OH)4: alternate stacking of tobermorite and rosenbuschite-like units Locality: skarndolomite xenoliths, Dovyren massif, Russia
American Mineralogist, 2008, 93, 456-462
9010400 CIFAs2 Cu1.87 H12 Mg3.13 O16P 1 21/c 15.459; 16.808; 6.917
90; 100.44; 90
624.162Kyono, A.
Compositional variability and crystal structural features of guanacoite
American Mineralogist, 2008, 93, 501-507
9010401 CIFMg O3 SiP 1 21/m 19.477; 6.205; 4.256
90; 98.75; 90
247.36Tschauner, O.; Kiefer, B.; Liu, H.; Sinogeikin, S.; Somayazulu, M.; Luo, S.-N.
Possible structural polymorphism in Al-bearing magnesiumsilicate post-perovskite Sample: 3X1
American Mineralogist, 2008, 93, 533-539
9010402 CIFMg O3 SiP 1 21/m 17.026; 6.228; 4.262
90; 95.85; 90
185.525Tschauner, O.; Kiefer, B.; Liu, H.; Sinogeikin, S.; Somayazulu, M.; Luo, S.-N.
Possible structural polymorphism in Al-bearing magnesiumsilicate post-perovskite Sample: 2X1 Note: atom sites modified after communication with author
American Mineralogist, 2008, 93, 533-539
9010403 CIFFe2 O9 Pb2 Si2P b c n6.9788; 11.0164; 10.0881
90; 90; 90
775.586Dorsam, G.; Liebscher, A.; Wunder, B.; Franz, G.
Crystal structures of synthetic melanotekite (Pb2Fe2Si2O9), kentrolite (Pb2Mn2Si2O9), and the aluminum analogue (Pb2Al2Si2O9)
American Mineralogist, 2008, 93, 573-583
9010404 CIFMn2 O9 Pb2 Si2P 21 2 217.0079; 11.0665; 9.9634
90; 90; 90
772.691Dorsam, G.; Liebscher, A.; Wunder, B.; Franz, G.
Crystal structures of synthetic melanotekite (Pb2Fe2Si2O9), kentrolite (Pb2Mn2Si2O9), and the aluminum analogue (Pb2Al2Si2O9)
American Mineralogist, 2008, 93, 573-583
9010405 CIFAl2 O9 Pb2 Si2P b c n6.8981; 10.6906; 9.7413
90; 90; 90
718.37Dorsam, G.; Liebscher, A.; Wunder, B.; Franz, G.
Crystal structures of synthetic melanotekite (Pb2Fe2Si2O9), kentrolite (Pb2Mn2Si2O9), and the aluminum analogue (Pb2Al2Si2O9)
American Mineralogist, 2008, 93, 573-583
9010406 CIFFe H O2P b n m4.6163; 9.9564; 3.0248
90; 90; 90
139.025Alvarez, M.; Sileo, E. E.; Rueda, E. H.
Structure and reactivity of synthetic Co-substituted goethites Sample: G0, 0 mol% Co Note: changed OH(x) to match reported bond distances
American Mineralogist, 2008, 93, 584-590
9010407 CIFCo0.03 Fe0.97 H O2P b n m4.607; 9.9472; 3.021
90; 90; 90
138.443Alvarez, M.; Sileo, E. E.; Rueda, E. H.
Structure and reactivity of synthetic Co-substituted goethites Sample: G3, 3 mol% Co
American Mineralogist, 2008, 93, 584-590
9010408 CIFCo0.05 Fe0.95 H O2P b n m4.5975; 9.9395; 3.0183
90; 90; 90
137.927Alvarez, M.; Sileo, E. E.; Rueda, E. H.
Structure and reactivity of synthetic Co-substituted goethites Sample: G5, 5 mol% Co Note: changed O(x) to match reported bond distances
American Mineralogist, 2008, 93, 584-590
9010409 CIFCo0.07 Fe0.93 H O2P b n m4.5901; 9.9309; 3.0148
90; 90; 90
137.426Alvarez, M.; Sileo, E. E.; Rueda, E. H.
Structure and reactivity of synthetic Co-substituted goethites Sample: G7, 7 mol% Co
American Mineralogist, 2008, 93, 584-590
9010410 CIFCo0.1 Fe0.9 H O2P b n m4.58; 9.9198; 3.0102
90; 90; 90
136.761Alvarez, M.; Sileo, E. E.; Rueda, E. H.
Structure and reactivity of synthetic Co-substituted goethites Sample: G10, 10 mol% Co
American Mineralogist, 2008, 93, 584-590
9010411 CIFH2 Mg1.864 O4.129 SiI 1 2/m 15.6807; 11.5243; 8.2515
90; 90.09; 90
540.193Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J.
Effects of hydration on the structure and compressibility of wadsleyite, beta-(Mg2SiO4) Locality: synthetic Sample: SS0401, 1.66 wt% H2O
American Mineralogist, 2008, 93, 598-607
9010412 CIFH2 Mg1.89 O4.092 SiI m m a5.6862; 11.5023; 8.2526
90; 90.013; 90
539.756Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J.
Effects of hydration on the structure and compressibility of wadsleyite, beta-(Mg2SiO4) Locality: synthetic Sample: SS0402, 1.18 wt% H2O
American Mineralogist, 2008, 93, 598-607
9010413 CIFH2 Mg1.961 O4.03 SiI m m a5.6951; 11.4628; 8.2565
90; 90.001; 90
538.999Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J.
Effects of hydration on the structure and compressibility of wadsleyite, beta-(Mg2SiO4) Locality: synthetic Sample: SS0403, 0.38 wt% H2O
American Mineralogist, 2008, 93, 598-607
9010414 CIFMg2 O4 SiI m m a5.7008; 11.4407; 8.2582
90; 90; 90
538.609Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J.
Effects of hydration on the structure and compressibility of wadsleyite, beta-(Mg2SiO4) Sample: WS3056, 0.005 wt% H2O
American Mineralogist, 2008, 93, 598-607
9010415 CIFAl1.229 Fe0.781 H1.186 K Mg2.219 O12 Si2.704C 1 2/m 15.3278; 9.2225; 10.2087
90; 100.031; 90
493.943Ventruti, G.; Zema, M.; Scordari, F.; Pedrazzi, G.
Thermal behavior of a Ti-rich phlogopite from Mt. Vulture (Potenza, Italy): An in situ X-ray single-crystal diffraction study Sample: T = 100 K
American Mineralogist, 2008, 93, 632-643
9010416 CIFAl1.227 Fe0.799 H1.189 K Mg2.201 O12 Si2.699C 1 2/m 15.331; 9.2298; 10.2217
90; 100.031; 90
495.261Ventruti, G.; Zema, M.; Scordari, F.; Pedrazzi, G.
Thermal behavior of a Ti-rich phlogopite from Mt. Vulture (Potenza, Italy): An in situ X-ray single-crystal diffraction study Sample: T = 200 K
American Mineralogist, 2008, 93, 632-643
9010417 CIFAl1.226 Fe0.797 H1.187 K Mg2.203 O12 Si2.698C 1 2/m 15.3365; 9.2438; 10.2331
90; 100.031; 90
497.078Ventruti, G.; Zema, M.; Scordari, F.; Pedrazzi, G.
Thermal behavior of a Ti-rich phlogopite from Mt. Vulture (Potenza, Italy): An in situ X-ray single-crystal diffraction study Sample: T = 298 K
American Mineralogist, 2008, 93, 632-643
9010418 CIFAl1.224 Fe0.785 K Mg2.215 O12 Si2.693C 1 2/m 15.316; 9.2043; 10.1613
90; 100.06; 90
489.549Ventruti, G.; Zema, M.; Scordari, F.; Pedrazzi, G.
Thermal behavior of a Ti-rich phlogopite from Mt. Vulture (Potenza, Italy): An in situ X-ray single-crystal diffraction study Sample: T = 298 K after reversal experiment
American Mineralogist, 2008, 93, 632-643

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