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-BI16
Locality:Middle Atlas Neogene-Quaternary Volcanic Field of Morocco
_database_code_amcsd 0020063
8.2021 8.2021 8.2021 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 .714  .0046  .0046  .0046  .0046       0       0       0
FeT    .125   .125   .125 .287  .0046  .0046  .0046  .0046       0       0       0
AlM      .5     .5     .5 .603 .00325 .00325 .00325 .00325 -.00043 -.00043 -.00043
CrM      .5     .5     .5 .397 .00325 .00325 .00325 .00325 -.00043 -.00043 -.00043
O    .26275 .26275 .26275      .00615 .00615 .00615 .00615 -.00079 -.00079 -.00079
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