Crystallography Open Database

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9017033 CIFAl1.718 Cr0.282 Fe0.24 Mg0.76 O4F d -3 m :28.1339; 8.1339; 8.1339
90; 90; 90		538.142Lenaz, 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-TF6
American Mineralogist, 2014, 99, 267-275
9017034 CIFAl1.76 Cr0.24 Fe0.236 Mg0.764 O4F d -3 m :28.1351; 8.1351; 8.1351
90; 90; 90		538.38Lenaz, 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-TF7
American Mineralogist, 2014, 99, 267-275
9017035 CIFAl1.42 Cr0.58 Fe0.3 Mg0.7 O4F d -3 m :28.1704; 8.1704; 8.1704
90; 90; 90		545.419Lenaz, 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-TF8
American Mineralogist, 2014, 99, 267-275
9017036 CIFAl1.6 Cr0.4 Fe0.268 Mg0.732 O4F d -3 m :28.1391; 8.1391; 8.1391
90; 90; 90		539.174Lenaz, 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-TF21
American Mineralogist, 2014, 99, 267-275
9017037 CIFAl1.612 Cr0.388 Fe0.234 Mg0.766 O4F d -3 m :28.1499; 8.1499; 8.1499
90; 90; 90		541.323Lenaz, 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-TF28
American Mineralogist, 2014, 99, 267-275

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All data in the COD and the database itself are dedicated to the public domain and licensed under the CC0 License . Users of the data should acknowledge the original authors of the structural data.