| Reference Type | Journal (article/letter/editorial) |
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| Title | Pyroxenes and coexisting minerals in the Cheviot granite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Haslam, H. W. | Author |
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| Year | 1986 (December) | Volume | 50 |
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| Issue | 358 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_50/50-358-671.pdf+ |
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| DOI | doi:10.1180/minmag.1986.050.358.13Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3912 | Long-form Identifier | mindat:1:5:3912:7 |
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| GUID | 0 |
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| Full Reference | Haslam, H. W. (1986) Pyroxenes and coexisting minerals in the Cheviot granite. Mineralogical Magazine, 50 (358) 671-674 doi:10.1180/minmag.1986.050.358.13 |
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| Plain Text | Haslam, H. W. (1986) Pyroxenes and coexisting minerals in the Cheviot granite. Mineralogical Magazine, 50 (358) 671-674 doi:10.1180/minmag.1986.050.358.13 |
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| In | (1986, December) Mineralogical Magazine Vol. 50 (358) Mineralogical Society |
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| Abstract/Notes | AbstractOrthopyroxene and clinopyroxene, with biotite, are widespread in the high-level Cheviot granite, while amphibole is rare. The pyroxene compositions are very close to (Mg,Fe)2Si2O6 and Ca(Mg,Fe)Si2O6. Biotite compositions, with low Si and Al, are characteristic of biotites coexisting with pyroxenes. Geothermometric estimates based on oxide and pyroxene compositions show that present mineral compositions result from post-consolidation equilibration. |
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