| Reference Type | Journal (article/letter/editorial) |
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| Title | Serpentine minerals from veins in serpentinite rocks |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Morandi, N. | Author |
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| Felice, G. | Author |
| Year | 1979 (March) | Volume | 43 |
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| Issue | 325 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-325-135.pdf+ |
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| DOI | doi:10.1180/minmag.1979.043.325.13Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2991 | Long-form Identifier | mindat:1:5:2991:3 |
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| GUID | 0 |
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| Full Reference | Morandi, N., Felice, G. (1979) Serpentine minerals from veins in serpentinite rocks. Mineralogical Magazine, 43 (325) 135-140 doi:10.1180/minmag.1979.043.325.13 |
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| Plain Text | Morandi, N., Felice, G. (1979) Serpentine minerals from veins in serpentinite rocks. Mineralogical Magazine, 43 (325) 135-140 doi:10.1180/minmag.1979.043.325.13 |
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| In | (1979, March) Mineralogical Magazine Vol. 43 (325) Mineralogical Society |
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| Abstract/Notes | SummaryCrystal-chemical analyses of the serpentine polymorphs, sampled from macroscopic veins in the serpentinite rocks from Sasso della Mantesca and Sasso di S. Zanobi, are reported. The samples were examined by X-ray diffraction, thermal analysis (TG and DTG), scanning and transmission electron microscopy, IR absorption spectroscopy, microprobe, and chemical tests.The results show: chrysotile 2Orc1 in tubular fibrils placed perpendicularly to walls of iso-oriented ‘lenticular veins’; and polygonal serpentine formed by flat layers of lizardite 2H and/or 1T, arranged as an outer shell of a central core of chrysotile 2Mc1 fibres; this type of serpentine with high crystallinity and unusual morphological development is included in ‘green veins’, which show variable Al, Fe, and Mg contents.A genetic mechanism correlating the petrographic observations with the mineralogical results is discussed. |
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