| Reference Type | Journal (article/letter/editorial) |
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| Title | A garnierite with a high nickel content from Western Australia |
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| Journal | Mineralogical Magazine |
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| Authors | Nickel, E. H. | Author |
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| Bridge, P. J. | Author |
| Year | 1975 (March) | Volume | 40 |
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| Issue | 309 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_40/40-309-65.pdf+ |
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| DOI | doi:10.1180/minmag.1975.040.309.09Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 6830 | Long-form Identifier | mindat:1:5:6830:1 |
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| GUID | 0 |
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| Full Reference | Nickel, E. H., Bridge, P. J. (1975) A garnierite with a high nickel content from Western Australia. Mineralogical Magazine, 40 (309) 65-69 doi:10.1180/minmag.1975.040.309.09 |
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| Plain Text | Nickel, E. H., Bridge, P. J. (1975) A garnierite with a high nickel content from Western Australia. Mineralogical Magazine, 40 (309) 65-69 doi:10.1180/minmag.1975.040.309.09 |
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| In | (1975, March) Mineralogical Magazine Vol. 40 (309) Mineralogical Society |
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| Abstract/Notes | SummaryThe garnierite, which occurs in the oxide zone overlying a nickel sulphide deposit, consists of talc-like and serpentine-like components, with the former predominating. Chemical and electron-probe analyses give NiO contents ranging between 39.6 and 43.9 weight %. |
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