Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 26
... eastern part , by more than a mile . A similar situation is seen in the volcanic rocks near Paloga where the southern limit extends 14 miles more on the western bank than on the eastern . However , it is also possible that this ...
... eastern part , by more than a mile . A similar situation is seen in the volcanic rocks near Paloga where the southern limit extends 14 miles more on the western bank than on the eastern . However , it is also possible that this ...
Page 35
... eastern face . It supports thin and scattered vegetation except in a limited area around Pir Than where pine trees are grown . Due to dearth of water inhabitation is sporadic . The foundation of the eastern abutment of the earth fill ...
... eastern face . It supports thin and scattered vegetation except in a limited area around Pir Than where pine trees are grown . Due to dearth of water inhabitation is sporadic . The foundation of the eastern abutment of the earth fill ...
Page 38
... 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 chemically analysed for phosphate . Out of 35 samples ...
... 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 chemically analysed for phosphate . Out of 35 samples ...
Contents
Preliminary geology and petrography of Swat Kohistan | 1 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
Lithological classification and environment of deposition of | 43 |
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Common terms and phrases
abundant altered amphibolites appears associated bands base beds biotite body brown Bull chlorite colour common complex concentration consist contain correlated cover crystalline crystals dark deposits developed diorites distance dykes east eastern epidote exposed extend feet feldspar folded foliation Formation fractures Gandghar Range garnet Geol geology gneisses grades grains granites green grey Group Hazara hornblende inches Indus intrusions iron Kalam Kohistan latter layers light limestone locally located Lower marble material Member metals Middle miles minerals minor natural norites occur outcrop Pakistan pegmatite Peshawar phyllites places plagioclase present probably quartz quartzites rare region result River road rocks samples schists seen sericite shale shear slates solubility solutions southern stream strike structure suggest sulphide Swat temperature thick thin transport types Univ Upper usually valley varieties various veins village volcanic waters western zone