| Reference Type | Journal (article/letter/editorial) |
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| Title | Study of minerals from the pegmatites of the Nellore mica-belt, Andhra Pradesh, India Part I. Microcline perthites |
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| Journal | Mineralogical Magazine |
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| Authors | Babu, V. R. R. M. | Author |
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| Year | 1969 (March) | Volume | 37 |
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| Issue | 285 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-285-135.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.285.14Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6241 | Long-form Identifier | mindat:1:5:6241:5 |
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| GUID | 0 |
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| Full Reference | Babu, V. R. R. M. (1969) Study of minerals from the pegmatites of the Nellore mica-belt, Andhra Pradesh, India Part I. Microcline perthites. Mineralogical Magazine, 37 (285) 135-139 doi:10.1180/minmag.1969.037.285.14 |
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| Plain Text | Babu, V. R. R. M. (1969) Study of minerals from the pegmatites of the Nellore mica-belt, Andhra Pradesh, India Part I. Microcline perthites. Mineralogical Magazine, 37 (285) 135-139 doi:10.1180/minmag.1969.037.285.14 |
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| In | (1969, March) Mineralogical Magazine Vol. 37 (285) Mineralogical Society |
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| Abstract/Notes | SummaryThe obliquity values of microcline perthites are nearer to maximum microcline type, indicating that they have less than 10% Ab in their lattices, apart from exsolved albite. The perthites are classified based on form as stringlet, string, film, vein, and replacement types. It is concluded that stringlet and string perthites are formed by exsolution along contraction cracks, followed by film as a result of decrease in rate of cooling and increase in water vapour content of the pegmatites, whereas vein and replacement perthites are formed last, by replacement when the pegmatites crystallized in a closed system. Based on the chemical composition of microcline perthites, a temperature of 600 °C is arrived at for unmixing of feldspar to give rise to microcline perthite. |
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