The Genesis of the Quaternary Deposits Of The Vale of Peshawar, South of Kabul River by Inam Ullah Khan

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dc.contributor.authorInam Ullah Khan
dc.contributor.authorSupervised By: Prof. Dr. M. Said
dc.date.accessioned2026-07-29T05:11:52Z
dc.date.available2026-07-29T05:11:52Z
dc.date.issued1990
dc.description.abstractThe vale of Peshawar is located in the world's youngest Collision zone in the north-west of Pakistan. It remained a locus of various tectonic and geomorphological The present basin which was filled in with a variety of sediments,during the Quaternary period has been carved out of - | Tertiary mountain system as a result of Jong phases of erosion se | which lasted for about 15 to 19 m.y.8. The study area which is located South of the river Kabul forms an integral part of the : vale and possesses a complete- a record of such tectonic and geomorphological episodes which are preserved in various litho-stratigraphic units and exposed in different sections along the channels of present torrents draining the northern slopes of the Attock-Cherat range.
dc.identifier.urihttp://repository.uop.edu.pk/123456789/515
dc.language.isoen
dc.publisherDepartment of Geography
dc.relation.ispartofseries100066
dc.titleThe Genesis of the Quaternary Deposits Of The Vale of Peshawar, South of Kabul River by Inam Ullah Khan
dc.typeThesis
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