Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 26
bank do not extend on the eastern side which is occupied by diorites of different
appearance and texture . It can thus be assumed that a fault runs along the
stream to the south of Dewangar . Consequently , the western part of the valley
having ...
bank do not extend on the eastern side which is occupied by diorites of different
appearance and texture . It can thus be assumed that a fault runs along the
stream to the south of Dewangar . Consequently , the western part of the valley
having ...
Page 35
The eastern drainage is captured by Dor and Haro rivers through numerous
seasonal khwars which ultimately carry the water to Indus . The Gandghar Range
varies in elevations from less than 1 , 500 feet near the extreme ends , the north
and ...
The eastern drainage is captured by Dor and Haro rivers through numerous
seasonal khwars which ultimately carry the water to Indus . The Gandghar Range
varies in elevations from less than 1 , 500 feet near the extreme ends , the north
and ...
Page 38
One such occurrence has been located near Choi , on the eastern slope of Pir
Than peak . Heamatite and limonite are the iron ores associated with the
ferruginous bands . Their development is thin and erratic . • Pir Than Limestone
has been ...
One such occurrence has been located near Choi , on the eastern slope of Pir
Than peak . Heamatite and limonite are the iron ores associated with the
ferruginous bands . Their development is thin and erratic . • Pir Than Limestone
has been ...
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Contents
Preliminary geology and petrography of Swat Kohistan EARTH | 1 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
Lithological classification and environment of deposition of | 43 |
6 other sections not shown
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Common terms and phrases
abundant amounts amphibolites appears associated bands base beds biotite body brines Bull carbonates changes chlorite colour common complexes composition concentration contain correlated crystals dark deposits developed diorites dykes east eastern epidote exposed extend feet feldspar fluids folded Formation fractures Gandghar Range Geol geology grades grains granites green grey Group hornblende hydrothermal inclusions increases Indus intrusions iron Kalam latter layers light limestone locally located Lower marble material Member metals Middle miles minerals nature norites occur origin outcrop Pakistan pegmatite Peshawar phyllites places plagioclase present probably quartz quartzite rare region result River road rocks samples schists seen sericite shale sheared shown Slates solubility solutions stream strike structure suggested sulphide sulphur Swat temperature thick thin transport types Univ Upper usually valley varieties various veins village volcanic waters western zone