Recent Observation on the Undifferentiated Attock Group

Authors

  • R. A. Khan Tahirkheli National Centre of Excellence in Geology, University of Peshawar, Pakistan

Abstract

Under the light of recent invetigations, the Attock Slates are found to certain five distinct lithological units which are easilty differentiated in the field and belong to different ages. Three of these units are dated to be Upper Mesozoic, one is assigned a pre-Cambrian age and the fifth unit is still under observation and is tentively placed in Paleozoic. The argillaceous part of the Attock Group which was previously considered to be one homogeneous unit is split into two divisions and named "Manki Slates" and "Dag Slates." The later contain fossilized bands of limestone and on the basis of diagnostic fossil (Cerithiopsidea), have been dated to be Upper Cretaceous age. These two slates have got tectonic contact and the older Manki slates are found to have thrust over the younger Dag slates.

References

Ahmad, Mesbahuddin, 1965. Personal Communication.

Cotter, G. de P., 1933. The geology of part of the Attock District West of longitude 75o45'E. Memoirs of Geological Survey of India, 2, 63-161.

Middlemiss, C.S., 1896. The geology of Hazara and Black Mountains. Memoirs of Geological Survey of India, 26(1), 1-290.

Mohammad Ali, Ch., 1962. The stratigraphy of the southern Tanol Area, Hazara, West Pakistan. Geological Bulletin of Panjab University, 2, 31-40.

Wynne, A.B., 1873. Notes from a progress report on hte geology of parts of the upper Panjab. Records of Geological Survey of India, 3, 59-64.

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Published

1965-12-31

How to Cite

Tahirkheli, R. A. K. (1965). Recent Observation on the Undifferentiated Attock Group. Journal of Himalayan Earth Sciences, 2(2), 10-23. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1066

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