| Reference Type | Journal (article/letter/editorial) |
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| Title | Amphiboles and biotite in relation to the stages of metamorphism in granogabbro |
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| Journal | Mineralogical Magazine |
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| Authors | Smulikowski, W. | Author |
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| Year | 1974 (December) | Volume | 39 |
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| Issue | 308 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-308-857.pdf+ |
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| DOI | doi:10.1180/minmag.1974.039.308.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6807 | Long-form Identifier | mindat:1:5:6807:3 |
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| GUID | 0 |
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| Full Reference | Smulikowski, W. (1974) Amphiboles and biotite in relation to the stages of metamorphism in granogabbro. Mineralogical Magazine, 39 (308) 857-866 doi:10.1180/minmag.1974.039.308.05 |
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| Plain Text | Smulikowski, W. (1974) Amphiboles and biotite in relation to the stages of metamorphism in granogabbro. Mineralogical Magazine, 39 (308) 857-866 doi:10.1180/minmag.1974.039.308.05 |
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| In | (1974, December) Mineralogical Magazine Vol. 39 (308) Mineralogical Society |
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| Abstract/Notes | SummaryThe Bratteggdalen granogabbro, a relict mass in the Caledonian amphibolites of Vestspitsbergen, shows a series of amphibole development reflecting its thermal history. A brown Ti-rich hornblende occurs as a late magmatic mantling of pyroxene. Low-grade metamorphism (greenschist facies) was accompanied by the development of actinolite from pyroxene; subsequent amphibolite facies metamorphism saw the development of an alkali-rich, blue-green hornblende. The chemical changes in the amphiboles are a succinct illustration of those found in progressive regional metamorphism. |
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