Reference Type | Journal (article/letter/editorial) |
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Title | A tholeiitic phase of the quartz-dolerite magma of central Scotland |
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Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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Authors | Walker, Frederick | Author |
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Year | 1930 (September) | Volume | 22 |
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Issue | 130 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_22/22-130-368.pdf+ |
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DOI | doi:10.1180/minmag.1930.22.130.02 |
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| Generate Citation Formats |
Mindat Ref. ID | 7101 | Long-form Identifier | mindat:1:5:7101:1 |
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GUID | 0 |
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Full Reference | Walker, Frederick (1930) A tholeiitic phase of the quartz-dolerite magma of central Scotland. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (130) 368-376 doi:10.1180/minmag.1930.22.130.02 |
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Plain Text | Walker, Frederick (1930) A tholeiitic phase of the quartz-dolerite magma of central Scotland. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (130) 368-376 doi:10.1180/minmag.1930.22.130.02 |
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In | (1929) Mineralogical Magazine Vol. 22 (130) Mineralogical Society |
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Abstract/Notes | The Permo-Carboniferous quartz-dolerites of central Scotland are generally holocrystalline, and only two intrusions amongst them with a fresh vitreous base have been recorded—those of Dalmeny in West Lothian, andKinkellnear Kirkintilloch (northof Glasgow). Both rocks have already been described briefly, but in view of their many interesting features a more thorough treatment seems desirable, particularly as they have a bearing on some recent theories of magmatie differentiation advanced by Dr. C. N. Fenner. |
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