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Name: Stannoidite RRUFF ID: R160066 Ideal Chemistry: Cu8(Fe,Zn)3Sn2S12 Locality: Junction mine, Warren District, Cochise County, Arizona, USA Source: University of Arizona Mineral Museum 3169 [view label] Owner: RRUFF Description: Black grains in massive bornite and chalcopyrite matrix. Under optical microscope, stannoidite crystals are brownish. The gray-pinkish material is bornite and light-gray is chalcopyrite. Status: The identification of this mineral is confirmed by single-crystal X-ray diffraction and chemical analysis. |
Mineral Group: [ Stannoidite (1) ] |
CHEMISTRY | ||||||||||
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POWDER DIFFRACTION | |||||||
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RRUFF ID: | R160066.9 | ||||||
Sample Description: | Single crystal, powder profile is calculated | ||||||
Cell Refinement Output: |
a: 10.8217(9)Å b: 5.4103(7)Å c: 16.1121(20)Å alpha: 90° beta: 90° gamma: 90° Volume: 943.35(19)Å3 Crystal System: orthorhombic |
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REFERENCES for Stannoidite | |
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American Mineralogist Crystal Structure Database Record: [view record] |
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Anthony J W, Bideaux R A, Bladh K W, and Nichols M C (1990) Handbook of Mineralogy, Mineral Data Publishing, Tucson Arizona, USA, by permission of the Mineralogical Society of America. [view file] |
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Fleischer M (1969) New mineral names, American Mineralogist, 54, 1495-1499 [view file] |
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Kato A (1969) Stannoidite, Cu5(Fe, Zn)2SnS8, a new stannite-like mineral from the Konjo mine, Okayama Prefecture, Japan, Bulletin National Science Museum, Tokyo, 12, 165-172 [view file] |
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Kudoh Y, Takéuchi Y (1976) The superstructure of stannoidite, Zeitschrift für Kristallographie, 144, 145-160 [view file] |
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Taxer K (1981) Substructures and their application in crystal structure analysis, Zeitschrift für Kristallographie, 155, 1-25 [view file] |
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