Reference Type | Journal (article/letter/editorial) |
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Title | Microstructural interpretation of some fibrolitic sillimanite aggregates |
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Journal | Mineralogical Magazine |
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Authors | Vernon, R. H. | Author |
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Year | 1975 (September) | Volume | 40 |
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Issue | 311 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_40/40-311-303.pdf+ |
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DOI | doi:10.1180/minmag.1975.040.311.10Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6876 | Long-form Identifier | mindat:1:5:6876:9 |
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GUID | 0 |
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Full Reference | Vernon, R. H. (1975) Microstructural interpretation of some fibrolitic sillimanite aggregates. Mineralogical Magazine, 40 (311) 303-306 doi:10.1180/minmag.1975.040.311.10 |
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Plain Text | Vernon, R. H. (1975) Microstructural interpretation of some fibrolitic sillimanite aggregates. Mineralogical Magazine, 40 (311) 303-306 doi:10.1180/minmag.1975.040.311.10 |
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In | (1975, September) Mineralogical Magazine Vol. 40 (311) Mineralogical Society |
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Abstract/Notes | SummaryFibrolitic sillimanite in some high-grade gneisses from Broken Hill, Australia, shows microstructural features suggestive of compatibility with the main coarser-grained assemblage, namely: framework-silicate interfaces either meet (110)-sillimanite/framework-silicate interfaces at approximately 90° or are attached to the ends of 'fibrolite' rods; framework-silicate interfaces are deflected by 'fibrolite' grains; and interfaces of inclusions of one framework silicate in another are deflected by 'fibrolite' grains, producing irregular, rather than rounded, inclusion shapes. These criteria suggest that the 'fibrolite' in some rocks is a compatible member of the main metamorphic assemblage. Its persistence as small grains may be due to a high proportion of relatively low-energy prismatic boundaries in the fibrolitic aggregates. |
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