Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 3
... stream and elsewhere . In some cases , tbis change is due to end morains but in others it is due to high quantity of talus or alluvial fans . The latter are a common feature of the area although they are more so in the northernmost part ...
... stream and elsewhere . In some cases , tbis change is due to end morains but in others it is due to high quantity of talus or alluvial fans . The latter are a common feature of the area although they are more so in the northernmost part ...
Page 57
... stream near Ghakbai . It is a sharp contact with a shear zone in the hornblend - schist , about 50 feet thick . Some schist near the contact is granitized . About 150 feet away from the contact two parallel veins of hornblendite occur ...
... stream near Ghakbai . It is a sharp contact with a shear zone in the hornblend - schist , about 50 feet thick . Some schist near the contact is granitized . About 150 feet away from the contact two parallel veins of hornblendite occur ...
Page 75
... streams . Streams are quite broad in the western part of the area but are narrow in eastern and southeastern parts . The main streams of the area are Barang Nala , Ambabar Roa , Gandao Khwar , Pindiali Rud and Danish Kol Khwar . Running ...
... streams . Streams are quite broad in the western part of the area but are narrow in eastern and southeastern parts . The main streams of the area are Barang Nala , Ambabar Roa , Gandao Khwar , Pindiali Rud and Danish Kol Khwar . Running ...
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