A Skarn Rock from Dir, Northwest Pakistan

Authors

  • D.R.C. Kempe Deptt. of Mineralogy, British Museum (Natural History) London SW7 5BD, U.K
  • M. Qasim Jan National Centre of Excellence in Geology, University of Peshawar, Pakistan
  • G.C. Jones Deptt. of Mineralogy, British Museum (Natural History) London SW7 5BD, U.K
  • V.K. Din Deptt. of Mineralogy, British Museum (Natural History) London SW7 5BD, U.K

Abstract

The geology and petrology of a skarn from northwest Pakistan me presented. The chemistry of the rocks and their constituent minerals is discussed briefly and compared with other similar occurrences. The rock chemistry and the abundance of ferrosalite, andradite-rich garnet, and epidote (Fe3+/(Fe3+ + Al) = 0.30) are considered to be due to metasomatism (mainly the introduction of iron, and possibly silica) of the country metasediments or, less likely, volcanic rocks by a biotite-two pyroxene tonalite intrusion.

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Published

1985-03-30

How to Cite

Kempe, D., Jan, M. Q., Jones, G., & Din, V. (1985). A Skarn Rock from Dir, Northwest Pakistan. Journal of Himalayan Earth Sciences, 18(1), 103-111. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1287

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