American Mineralogist Crystal Structure Database

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Spinel
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Lenaz D, Youbi N, Min A D, Boumehdi M A, Abbou M B
American Mineralogist 99 (2014) 267-275
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
Locality:Middle Atlas Neogene-Quaternary Volcanic Field of Morocco
_database_code_amcsd 0020066
8.13510 8.13510 8.13510 90 90 90 *Fd3m
.125 .125 .125
atom      x      y      z  occ   Uiso U(1,1) U(2,2) U(3,3)  U(1,2)  U(1,3)  U(2,3)
MgT    .125   .125   .125 .764  .0060  .0060  .0060  .0060       0       0       0
FeT    .125   .125   .125 .236  .0060  .0060  .0060  .0060       0       0       0
AlM      .5     .5     .5 .880 .00408 .00408 .00408 .00408 -.00045 -.00045 -.00045
CrM      .5     .5     .5 .120 .00408 .00408 .00408 .00408 -.00045 -.00045 -.00045
O    .26283 .26283 .26283      .00737 .00737 .00737 .00737 -.00016 -.00016 -.00016
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