| Reference Type | Journal (article/letter/editorial) |
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| Title | The occurrence of eclogite on the Lyell Highway, Tasmania |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Spry, Alan | Author |
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| Year | 1963 (September) | Volume | 33 |
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| Issue | 262 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-262-589.pdf+ |
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| DOI | doi:10.1180/minmag.1963.033.262.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5750 | Long-form Identifier | mindat:1:5:5750:3 |
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| GUID | 0 |
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| Full Reference | Spry, Alan (1963) The occurrence of eclogite on the Lyell Highway, Tasmania. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (262) 589-593 doi:10.1180/minmag.1963.033.262.05 |
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| Plain Text | Spry, Alan (1963) The occurrence of eclogite on the Lyell Highway, Tasmania. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (262) 589-593 doi:10.1180/minmag.1963.033.262.05 |
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| In | (1962) Mineralogical Magazine Vol. 33 (262) Mineralogical Society |
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| Abstract/Notes | SummaryEclogite occurring about 20 miles east of Queenstown, Tasmania, is the first example of this kind of rock to be described in detail from Australia. It has the chemical composition of a basic igneous rock and consists of garnet (A115.8Fe‴0.6Fe″10.0Mg7.3Ca5.7Si24O96) and pyroxene (Ca4.5Na2.5Mg3.7Fe″0.7Fe‴0.4Ti0.1Aliv3.7Aliv0.7Si15.3O48)with amphibole, muscovite, zoisite, quartz, rutile, and pyrite. The eclogite consists of lenticular bodies within Precambrian garnetiferous schists. |
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These are possibly similar items as determined by title/reference text matching only.
