Crystallography Open Database

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Searching journal of publication like 'American Mineralogist' volume of publication is 92

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9010353 CIFAl2 Mg O4F d -3 m :27.9874; 7.9874; 7.9874
90; 90; 90
509.585Nestola, F.; Boffa Ballaran, T.; Balic-Zunic T; Princivalle, F.; Secco, L.; Dal Negro, A.
Comparative compressibility and structural behavior of spinel MgAl2O4 at high pressures: the independency on the degree of cation order Locality: Sri Lanka Sample: P = 8.027 GPa, disordered
American Mineralogist, 2007, 92, 1838-1843
9010354 CIFCa Ir O3C m c m3.13451; 9.87568; 7.29518
90; 90; 90
225.825Martin, C. D.; Smith, R. I.; Marshall, W. G.; Parise, J. B.
High-pressure structure and bonding in CaIrO3: the structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction Note: Ca(z) and O(y) changed to match normal structure Sample: T = 2.0 K, P = 1 bar
American Mineralogist, 2007, 92, 1912-1918
9010355 CIFCa Ir O3C m c m3.13493; 9.87709; 7.29562
90; 90; 90
225.901Martin, C. D.; Smith, R. I.; Marshall, W. G.; Parise, J. B.
High-pressure structure and bonding in CaIrO3: the structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction Note: Ca(z) and O(y) changed to match normal structure Sample: T = 100.0 K, P = 1 bar
American Mineralogist, 2007, 92, 1912-1918
9010356 CIFCa Ir O3C m c m3.13622; 9.88198; 7.29871
90; 90; 90
226.202Martin, C. D.; Smith, R. I.; Marshall, W. G.; Parise, J. B.
High-pressure structure and bonding in CaIrO3: the structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction Note: Ca(z) and O(y) changed to match normal structure Sample: T = 205.0 K, P = 1 bar
American Mineralogist, 2007, 92, 1912-1918
9010357 CIFCa Ir O3C m c m3.13645; 9.88352; 7.29903
90; 90; 90
226.264Martin, C. D.; Smith, R. I.; Marshall, W. G.; Parise, J. B.
High-pressure structure and bonding in CaIrO3: the structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction Note: Ca(z) and O(y) changed to match normal structure Sample: T = 293 K, P = 1 bar
American Mineralogist, 2007, 92, 1912-1918

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