Geology of the Baraul Valley, Dir

Authors

  • Jehanzeb Khan Federally Administered Tribal Areas Development Corporation, Peshawar.

Abstract

Over 520 sq. km. of the Baraul Valley has been investigated geologically and mapped on 1:63, 360 scale. Quartzite are the oldest rocks, exposed in the eastern part of the valley, and overlain by the mixed series of Palaeocene-Eocene age which covers the central part of the area. The series includes interbedded volcanics (andesite, dacite, rhyolite, tuff and agglomerates) and metasedimentary/sedimentary rocks (pelitic, calcarious and arenaceous) intruded by small post-Eocene dioritic rocks. A large part of the valley, in the north as well as the south, is occupied by ( ? ) Crete-Eocene diorites, quartz diorites, granodiorites and leucodiorites. The northern contact between the diorites and the mixed series is probably faulted.

References

Arbab, M. S. H. & Khan, R. N., 1973. Geology of Dir and northern part of Timurgara quadrangle, N. W. F. P., Pakistan. Geol. Surv. Pak., lnf. Rel. 49.

Chaudhry, M. N. & Chaudhry, A. G., 1974. Geology of Khagram area, Dir District. Geol. Bull, Punjab Univ., 11, 21-43.

Chaudhry, M. N., Kausar, A. B. & Lodhi, S. A. K., 1974. Geology of Timurgara-La1 Qila area Dir District, N. W. F. P. Geol. Bull. Punjab Univ., 11, 53-73.

Desto, A., 1974. Geological reconnaissance in the middle Indus valley between Chiles and Besham Qile (Pakistan), Bull. Soc. Geol. Ital., 93, 345-68.

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Published

1979-03-30

How to Cite

Khan, J. (1979). Geology of the Baraul Valley, Dir. Journal of Himalayan Earth Sciences, 11(1), 153-161. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1139