Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 26
... Indus Valley to investigate the potentials of the ultramafic rocks exposed Dear Jijal along the Indus River . Following is the result of the investigation : ( a ) Building and Decorative Material . Most of the Swat Kohistan is covered ...
... Indus Valley to investigate the potentials of the ultramafic rocks exposed Dear Jijal along the Indus River . Following is the result of the investigation : ( a ) Building and Decorative Material . Most of the Swat Kohistan is covered ...
Page 27
... Indus . ( b ) Abrasive Material . In the area between Patan and Jijal , along the Indus River , garnet gneisses are the most common rocks . Some of them have as much as 80 % garnet , besides plagioclase and ferromagneisan minerals . A ...
... Indus . ( b ) Abrasive Material . In the area between Patan and Jijal , along the Indus River , garnet gneisses are the most common rocks . Some of them have as much as 80 % garnet , besides plagioclase and ferromagneisan minerals . A ...
Page 35
... Indus valley on the west . The old Indus terraces on the western ilank of the Range form narrow strip between Tarbela and Ghazi villages , for a distance of about 12 miles . Downstream of Ghazi the Indus valley gradually widens and near ...
... Indus valley on the west . The old Indus terraces on the western ilank of the Range form narrow strip between Tarbela and Ghazi villages , for a distance of about 12 miles . Downstream of Ghazi the Indus valley gradually widens and near ...
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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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