| Reference Type | Journal (article/letter/editorial) |
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| Title | Variability within a saprolite deposit near Quebec City, Canada |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Kimpe, Christian De | Author |
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| Wang, Chang | Author |
| Laverdière, Marc | Author |
| LaSalle, Pierre | Author |
| Year | 1985 (May 1) | Volume | 22 |
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| Issue | 5 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e85-083Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 478683 | Long-form Identifier | mindat:1:5:478683:6 |
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| GUID | 0 |
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| Full Reference | Kimpe, Christian De, Wang, Chang, Laverdière, Marc, LaSalle, Pierre (1985) Variability within a saprolite deposit near Quebec City, Canada. Canadian Journal of Earth Sciences, 22 (5) 781-785 doi:10.1139/e85-083 |
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| Plain Text | Kimpe, Christian De, Wang, Chang, Laverdière, Marc, LaSalle, Pierre (1985) Variability within a saprolite deposit near Quebec City, Canada. Canadian Journal of Earth Sciences, 22 (5) 781-785 doi:10.1139/e85-083 |
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| In | (1985, May) Canadian Journal of Earth Sciences Vol. 22 (5) Canadian Science Publishing |
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| Abstract/Notes | Samples were collected in two trenches opened in a saprolite developed in a mylonite derived from biotite–garnet gneiss near Quebec City in order to investigate the spatial variability from the points of view of morphological, physical, mineralogical, and chemical properties. Phyllosilicate assemblages were: (a) kaolinite, (b) mica, (c) kaolinite + mica, and (d) mica + interstratified minerals (+ smectite). Grouping of the samples according to prominent colour in the matrix showed a relation between chroma and kaolinite content. Total chemical analyses were in good agreement with mineral assemblages. The spatial distribution of these assemblages corresponded to the degree of transformation of the gneiss into mylonite. |
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