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Myrmekite from the Charnockitic Rocks of the Eastern Ghats, India

Published online by Cambridge University Press:  01 May 2009

C. Bhattacharyya
Affiliation:
Department of Geology, Presidency CollegeCalcutta 12, India

Summary

The myrmekite occurring in acid to basic charnockites of the area around Garbham and Shikaruganji, Srikakulam district, Andhra Pradesh is described. Myrmekite, whenever present, occurs only at the contact of plagioclase and potash feldspar. The textures and paragenesis of minerals suggest that potash feldspar reacted with plagioclase giving rise to myrmekite under favourable stress condition, higher stress favouring the formation of myrmekite. The difference in the stress factor or the microstrain pattern in the rock can explain the presence of myrmekite at some contacts of plagioclase–potash feldspar and absence in others.

Type
Articles
Copyright
Copyright © Cambridge University Press 1971

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References

Becke, F. 1908. Uber myrmekit. Min. Pet. Mitt. 27, 377–91.Google Scholar
Carstens, H. 1967. Exsolution in ternary feldspars. II. Intergranular precipitation in alkali feldspar containing calcium in solid solution. Contr. Mineral. Petrol. 14, 316–20.CrossRefGoogle Scholar
Drescher-Kaden, F. K. 1948. Die feldspat-quartz-reaktiosgefüge der granite und gneiss und ihre genetische Bedeutung. Springer, Berlin.CrossRefGoogle Scholar
Hubbard, H. 1966. Myrmekite in charnockite from southwest Nigeria. Am. Miner. 51, 762–73.Google Scholar
Osterwald, F. W. 1955. Petrology of Precambrian granites in the northern Bighorn mountains, Wyoming. J. Geol. 63, 310–27.CrossRefGoogle Scholar
Phillips, E. R. 1964. Myrmekite and albite in some granites of the New England Batholith, New South Wales. J. geol. Soc. Aust. 11, 4960.CrossRefGoogle Scholar
Phillips, E. R. & Ransom, D. M. 1968. The proportionality of quartz in myrmekite. Am. Miner. 53, 1411–13.Google Scholar
Phillips, E. R. & Ransom, D. M. 1970. Myrmekite and non-myrmekitic plagioclase compositions in gneisses from Broken Hill, New South Wales. Mineralog. Mag. 37, 729–32.CrossRefGoogle Scholar
Ransom, D. M. & Phillips, E. R. 1969. The proportionality of quartz in myrmekite: A reply. Am. Miner. 54, 984–87.Google Scholar
Schwantke, A. 1909. Die Beimischung von Ca in Kalifeldspat und die Myrmekitbildung. Centralbl. Mineral Geol. 311–16.Google Scholar
Shelley, D. 1964. On myrmekites. Am. Miner. 49, 4152.Google Scholar
Shelley, D. 1969. The proportionality of quartz in myrmekite: A discussion. Am. Miner. 54, 982–4.Google Scholar
Shelley, D. 1970. The origin of myrmekitic intergrowths a comparison with rod-eutectics in metals. Mineralog. Mag. 37, 674–81.CrossRefGoogle Scholar