Hydrothermal Phenomenon Associated with Lahor Pegmatoid/Granite Complex, Kohistan

Authors

  • Khursheed Alam Butt Atomic Energy Minerals Centre, P.O. Box 734, University of Peshawar

Abstract

Pb-Zn-Mo and uranium mineralization spatially associated with Labor pegmatite/granite complex and enclosing metasediments is examined in the light of new data on ore minerals. Several ore paragenetic associations are described and it is concluded that polyphase mineralization processes are responsible for the ore associations described.

References

Ashraf, M., Chaudhry, M.N. and Hussain, S.S., 1980. Geology and economic significance of Lahor granite and rocks of southern ophiolite belt in Allai Kohistan area. Proc. Intern. Commit. Geodynamics, Grd 6. Mtg. Peshawar 1979. Spec. issue, Geol. Bull. Univ. Peshawar, 13, 207-213.

Butt, K.A. Arif, M., & Qarnar N.A., 1978. Evaluation of Uranium mineralization in pegmatoid rocks in Thakot and radiometric prospecting in adjoining areas. Unpublished report No. AEMC/EVZ, Atomic Energy Minerals Centre, Lahore.

Badham, J.P.N., Robinson, B.W., & Morton, R.D., 1972. The geology and genesis of Great Bear Lake silver deposit. 24th Internat. Geol. Congress. Section 4, 541-548.

Robinson, B.W. and Badham, J.P.N., 1974. Stable isotope geochemistry and the origin of Great Bear Lake silver deposits, N.W.T. Canada. Canadian Tour. Earth. Sci., 11, 698-711.

Robinson, B.W. and Ohmoto, H., 1973. Mineralogy, fluid inclusions and stable isotopes of the Echo bay U-Ni-Ag-Cu deposits, N.W.T. Canada. Econ. Geology, 68, 635-656.

Titley, S.R., and Hicks, C.L. (eds) 1966. Geology of porphyry copper deposits; south western North America. University of Arizona press, Tucson.

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Published

1981-03-30

How to Cite

Butt, K. A. (1981). Hydrothermal Phenomenon Associated with Lahor Pegmatoid/Granite Complex, Kohistan. Journal of Himalayan Earth Sciences, 14(1), 85-93. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1158