| Reference Type | Journal (article/letter/editorial) |
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| Title | On zoned associations of antigorite, talc, actinolite, chlorite, and biotite in Unst, Shetland Islands. |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Read, H. H. | Author |
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| Year | 1934 (June) | Volume | 23 |
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| Issue | 145 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_23/23-145-519.pdf+ |
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| DOI | doi:10.1180/minmag.1934.023.145.01 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 7182 | Long-form Identifier | mindat:1:5:7182:0 |
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| GUID | 0 |
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| Full Reference | Read, H. H. (1934) On zoned associations of antigorite, talc, actinolite, chlorite, and biotite in Unst, Shetland Islands. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (145) 519-540 doi:10.1180/minmag.1934.023.145.01 |
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| Plain Text | Read, H. H. (1934) On zoned associations of antigorite, talc, actinolite, chlorite, and biotite in Unst, Shetland Islands. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (145) 519-540 doi:10.1180/minmag.1934.023.145.01 |
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| In | (1932) Mineralogical Magazine Vol. 23 (145) Mineralogical Society |
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| Abstract/Notes | During my mapping for the Geological Survey in 1930 of the metamorphic rocks of western Unst, numerous small masses were encountered that were composed of a central part of talc followed outwards in order by zones of actinolite, chlorite, and biotite. Whilst revisiting the island in 1933 I was able to examine these associations in detail and to collect abundant material for study. As in many cases the zones are made up of a single mineral and may be a foot or so in thickness, specimens of great beauty are obtainable. |
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