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Epidiorite–limestone contact relations at Burawai, Hazara District, West Pakistan

Published online by Cambridge University Press:  14 March 2018

Summary

Special mineral assemblages in calcareous rocks 0–6 ft from the contact of an epidiorite sill are interpreted as the result of polymetamorphism–regional metamorphism superimposed on an earlier thermal metamorphism in which metasomatism, especially migration of potassium, was important.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1965

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References

Pascoe, (E. H.), 1950. A manual of the geology of India and Burma, 3rd ed., vol. 1. Government of india Press, Calcutta.Google Scholar
Rosenqvist, (I. TH.), 1952. The metamorphic facies and the feldspar minerals. Universitet i Bergen Årbok, vol. 4, p. 1.Google Scholar
Wadia, (D.N.), 1931. The syntaxis of the North-West Himalaya; its rocks, tectonics, and orogeny. Rec. Geol. Surv. India, vol. 65, p. 189.Google Scholar
Wadia, (D.N.), 1932. Note on the geology of Nanga Parbat (Mr. Diamir), and adjoining portions of Chi]as, Gilgit District, Kashmir. Ibid., vol. 66, p. 212.Google Scholar