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| 01935cam 2200313za 4500 |
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| 001 | 9.840670 |
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| 003 | CaOODSP |
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| 005 | 20221107151912 |
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| 007 | cr ||||||||||| |
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| 008 | 170731s1969 onca ob f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 043 | |an-cn--- |
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| 086 | 1 |aM38-8/78E-PDF|zM38-8/78 |
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| 100 | 1 |aNickel, Ernest H.,|d1925- |
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| 245 | 10|aStructural stability of minerals with the pyrite, marcasite, arsenopyrite and löllingite structures |h[electronic resource] / |cErnest H. Nickel, Mineral Sciences Division. |
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| 260 | |aOttawa : |bQueen's Printer, |c1969. |
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| 300 | |ap. [311]-321 : |bill. |
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| 490 | 1 |aReprint series ; |vRS 78 |
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| 500 | |aCover title. |
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| 500 | |a"Reprinted from The Canadian Mineralogist, vol. 9, part 3, 1968." |
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| 500 | |aHistorical publication digitized from print 2017 [by Natural Resources Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"The disulphides, diarsenides and sulpharsenides of iron, cobalt and nickel crystallize in structures characterized by "dumb-bells" of closely bound anion pairs (S-S or As-S), tetrahedral coordination of three cations and one anion around each anion, and octahedral coordination of six anions around each cation. However, there are significant differences between the various structures involved, and it is the purpose of this paper to investigate the relationship between composition and structure of these minerals, and to attempt to arrive at an explanation for this relationship"--Introd., p. [311]. |
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| 692 | 07|2gccst|aMinerals |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 1 |aCanada. |bDepartment of Energy, Mines and Resources. |
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| 710 | 1 |aCanada. |bMines Branch. |
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| 830 | #0|aReprint series - Dept. of Energy, Mines and Resources, Mines Branch ;|vRS 78|w(CaOODSP)9.834843 |
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| 856 | 40|qPDF|s1.71 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M38-8/M38-8-78-eng.pdf |
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