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American Mineralogist
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American Mineralogist; November-December 2009; v. 94; no. 11-12; p. 1727-1730; DOI: 10.2138/am.2009.3324
© 2009 Mineralogical Society of America
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Crystal structure of argentopyrite, AgFe2S3, and its relationship with cubanite

Hexiong Yang1,*, William W. Pinch2 and Robert T. Downs1

1 Department of Geosciences, University of Arizona, Tucson, Arizona 85721-0077, U.S.A.
2 19 Stonebridge Lane, Pittsford, New York, U.S.A.


Figure 1
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FIGURE 1. Comparison of crystal structures of (a) cubanite and (b) argentopyrite. The green and yellow tetrahedra represents MS4 and FeS4 groups (M = Cu for cubanite and Ag for argentopyrite), respectively. A three-member ring of tetrahedra in each structure is outlined with a circle, showing the positional difference of the MS4 tetrahedra.

 

Figure 2
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FIGURE 2. Comparison of the linkage among the FeS4 tetrahedra in (a) cubanite, (b) argentopyrite, (c) sternbergite, and (d) rasvumite.

 

Figure 3
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FIGURE 3. Cation ordering schemes in (a) cubanite, (b) high-temperature ordered phase of cubanite, proposed by Putnis (1977), and (c) argentopyrite. They are represented in terms of sulfur atoms coordinated by metal cations. Green, gray, and small yellow spheres represent M (=Cu in cubanite or Ag in argentopyrite), Fe, and S atoms, respectively.

 





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