| Reference Type | Journal (article/letter/editorial) |
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| Title | Paragenesis of the Minerals of the Three Component System MgO-Al2O3-SiO2 in Thermal Metamorphism |
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| Journal | Geological Magazine |
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| Authors | Tilley, C. E. | Author |
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| Year | 1923 (March) | Volume | 60 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800084727 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 280423 | Long-form Identifier | mindat:1:5:280423:5 |
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| GUID | 0 |
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| Full Reference | Tilley, C. E. (1923) Paragenesis of the Minerals of the Three Component System MgO-Al2O3-SiO2 in Thermal Metamorphism. Geological Magazine, 60 (3) 101-107 doi:10.1017/s0016756800084727 |
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| Plain Text | Tilley, C. E. (1923) Paragenesis of the Minerals of the Three Component System MgO-Al2O3-SiO2 in Thermal Metamorphism. Geological Magazine, 60 (3) 101-107 doi:10.1017/s0016756800084727 |
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| In | (1923, March) Geological Magazine Vol. 60 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | The system magnesia-alumina-silica is one of great importance in petrology, and the paragenesis of its constituent minerals must be a subject of study in any enquiry into the thermal metamorphism of rocks which have these three components as important constituents. Such rocks include particularly those of argillaceous type, magnesian-carbonate sediments, and bauxitic rocks. |
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