Powell, Derek (1966) On the preferred crystallographic orientation of garnet in some metamorphic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (276) 1094-1109 doi:10.1180/minmag.1966.036.276.05
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | On the preferred crystallographic orientation of garnet in some metamorphic rocks | ||
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society | ||
| Authors | Powell, Derek | Author | |
| Year | 1966 (December) | Volume | 36 |
| Issue | 276 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-276-1094.pdf+ | ||
| DOI | doi:10.1180/minmag.1966.036.276.05Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6019 | Long-form Identifier | mindat:1:5:6019:0 |
| GUID | 0 | ||
| Full Reference | Powell, Derek (1966) On the preferred crystallographic orientation of garnet in some metamorphic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (276) 1094-1109 doi:10.1180/minmag.1966.036.276.05 | ||
| Plain Text | Powell, Derek (1966) On the preferred crystallographic orientation of garnet in some metamorphic rocks. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (276) 1094-1109 doi:10.1180/minmag.1966.036.276.05 | ||
| In | (1966) Mineralogical Magazine Vol. 36 (276) Mineralogical Society | ||
| Abstract/Notes | SummaryA study of inclusions within garnet porphyroblasts demonstrates that planar inclusion bands and trails lie sub-parallel to one of the {110} planes of the host. The inclusions provide a relic of a rock fabric that existed before the growth of garnet. It is suggested that this fabric has determined the crystallographic orientation of garnet and may have arisen by the nucleation and epitaxial growth of garnet within or upon the mica lattice. | ||
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