| Reference Type | Journal (article/letter/editorial) |
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| Title | Inclusion patterns in zoned garnets from Magerøy, north Norway |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Andersen, T. B. | Author |
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| Year | 1984 (March) | Volume | 48 |
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| Issue | 346 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_48/48-346-21.pdf+ |
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| DOI | doi:10.1180/minmag.1984.048.346.03Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3583 | Long-form Identifier | mindat:1:5:3583:9 |
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| GUID | 0 |
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| Full Reference | Andersen, T. B. (1984) Inclusion patterns in zoned garnets from Magerøy, north Norway. Mineralogical Magazine, 48 (346) 21-26 doi:10.1180/minmag.1984.048.346.03 |
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| Plain Text | Andersen, T. B. (1984) Inclusion patterns in zoned garnets from Magerøy, north Norway. Mineralogical Magazine, 48 (346) 21-26 doi:10.1180/minmag.1984.048.346.03 |
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| In | (1984, March) Mineralogical Magazine Vol. 48 (346) Mineralogical Society |
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| Abstract/Notes | AbstractGarnet porphyroblasts in metasediments from Magerøy crystallized during static metamorphism. They display three optical zones, each having characteristic inclusions and chemistry. The compositional zoning is related to prograde metamorphism (an inner zone, 1, and a graphite-bearing zone) and retrogression (the outer zone, 2). Inclusions of two types are present in zone 1: type 1 are equidimensional remnants of the matrix, preferentially included along planes of rapid growth; type 2 are tubular and represent recrystallized quartz grains concentrated along defects in the garnet lattice. The defects are lineage boundaries between growth segments related to screw dislocations on crystal faces. Crystal growth developed at relatively high degrees of supersaturation, but below the supersaturation required for the development of dendrites. The inclusions suggest rapid growth of zone 1, caused by heat flow from an adjacent interkinematic mafic/ultramafic intrusive complex. The graphite-bearing zone crystallized at the metamorphic peak, while the inclusion-free idioblasfic rim probably developed during retrograde metamorphism. |
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