Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-02T20:19:26.641Z Has data issue: false hasContentIssue false
  • English
  • Français

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

Published online by Cambridge University Press:  14 March 2018

Get access Rights & Permissions [Opens in a new window]

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
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 34 , Issue 268 , 1965 , pp. 82 - 91
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1965

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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