Reference Type | Journal (article/letter/editorial) |
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Title | Subsilicic sodium gedrite in leptite of quartz keratophyric origin, Nordmark (Sweden) |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Linthout, Kees | Author |
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Lustenhouwer, Wim J. | Author |
Year | 1996 (April) | Volume | 60 |
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Issue | 399 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_60/60-399-379.pdf+ |
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DOI | doi:10.1180/minmag.1996.060.399.13Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 37 | Long-form Identifier | mindat:1:5:37:0 |
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|
GUID | 0 |
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Full Reference | Linthout, Kees, Lustenhouwer, Wim J. (1996) Subsilicic sodium gedrite in leptite of quartz keratophyric origin, Nordmark (Sweden) Mineralogical Magazine, 60 (399) 379-387 doi:10.1180/minmag.1996.060.399.13 |
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Plain Text | Linthout, Kees, Lustenhouwer, Wim J. (1996) Subsilicic sodium gedrite in leptite of quartz keratophyric origin, Nordmark (Sweden) Mineralogical Magazine, 60 (399) 379-387 doi:10.1180/minmag.1996.060.399.13 |
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In | (1996, April) Mineralogical Magazine Vol. 60 (399) Mineralogical Society |
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Abstract/Notes | The Mg—Fe orthoamphibole series □ (Mg, Fe)7Si8O22(OH)2 — Na(Mg, Fe)5- Al2Si5Al3O22(OH)2 has an open end in the sense that the Si5 end member has not been found in nature; tiny domains of near end–member composition in intricately zoned crystals (Schumacher, 1980; Robinson et al. 1982), appeared to be intergrowths of two different double-chain silicates (Schumacher, pers. comm., 1994). |
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