Crystallography Open Database

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COD ID Blue up arrow Links Formula Up arrow Space group Up arrow Cell parameters Cell volume Up arrow Bibliography
9017028 CIFAl1.94 Fe0.01 Mg0.38 Mn0.15 O4 Zn0.52F d -3 m :28.1123; 8.1123; 8.1123
90; 90; 90
533.866Halenius, U.; Bosi, F.
Color of Mn-bearing gahnite: A first example of electronic transitions in heterovalent exchange coupled IVMn2±VIMn3+ pairs in minerals.
American Mineralogist, 2014, 99, 261-266
9017029 CIFAl1.758 Cr0.242 Fe0.242 Mg0.758 O4F d -3 m :28.1334; 8.1334; 8.1334
90; 90; 90
538.042Lenaz, D.; Youbi, N.; Min, A. D.; Boumehdi, M. A.; Abbou, M. B.
Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle AtlasNeogene-Quaternary Volcanic Field (Morocco):Mineralogical evidence of a cooler mantle beneath the West African Craton. Note:Sample MAR-BI2
American Mineralogist, 2014, 99, 267-275
9017030 CIFAl1.6 Cr0.4 Fe0.25 Mg0.75 O4F d -3 m :28.1454; 8.1454; 8.1454
90; 90; 90
540.427Lenaz, D.; Youbi, N.; Min, A. D.; Boumehdi, M. A.; Abbou, M. B.
Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle AtlasNeogene-Quaternary Volcanic Field (Morocco):Mineralogical evidence of a cooler mantle beneath the West African Craton. Note:Sample MAR-BI4
American Mineralogist, 2014, 99, 267-275
9017031 CIFAl1.206 Cr0.794 Fe0.287 Mg0.714 O4F d -3 m :28.2021; 8.2021; 8.2021
90; 90; 90
551.792Lenaz, D.; Youbi, N.; Min, A. D.; Boumehdi, M. A.; Abbou, M. B.
Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle AtlasNeogene-Quaternary Volcanic Field (Morocco):Mineralogical evidence of a cooler mantle beneath the West African Craton. Note:Sample MAR-BI16
American Mineralogist, 2014, 99, 267-275
9017032 CIFAl1.38 Cr0.62 Fe0.306 Mg0.694 O4F d -3 m :28.1727; 8.1727; 8.1727
90; 90; 90
545.879Lenaz, D.; Youbi, N.; Min, A. D.; Boumehdi, M. A.; Abbou, M. B.
Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle AtlasNeogene-Quaternary Volcanic Field (Morocco):Mineralogical evidence of a cooler mantle beneath the West African Craton. Note:Sample MAR-BI24
American Mineralogist, 2014, 99, 267-275

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