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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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Reference TypeJournal (article/letter/editorial)
TitleThe occurrence of eclogite on the Lyell Highway, Tasmania
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsSpry, AlanAuthor
Year1963 (September)Volume33
Issue262
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_33/33-262-589.pdf+
DOIdoi:10.1180/minmag.1963.033.262.05Search in ResearchGate
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Mindat Ref. ID5750Long-form Identifiermindat:1:5:5750:3
GUID0
Full ReferenceSpry, 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
Plain TextSpry, 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
In(1962) Mineralogical Magazine Vol. 33 (262) Mineralogical Society
Abstract/NotesSummaryEclogite 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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