Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 23
... western side of Ushu Gol ( Matsushita , 1965 ) . The two sides were thus regarded to be faulted . According to our observations at a few places on the western bank , the trend of the foliation as well as of the metasedimentary beds ...
... western side of Ushu Gol ( Matsushita , 1965 ) . The two sides were thus regarded to be faulted . According to our observations at a few places on the western bank , the trend of the foliation as well as of the metasedimentary beds ...
Page 26
... western tributary . Because of extreme relief , the contact between the volcanic rocks and the Basic Complex has not been carefully studied . cases Matsushita and Huzita ( 1966 ) pointed out that " the geological structure of the Western ...
... western tributary . Because of extreme relief , the contact between the volcanic rocks and the Basic Complex has not been carefully studied . cases Matsushita and Huzita ( 1966 ) pointed out that " the geological structure of the Western ...
Page 35
... 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 Ghurghushti plain stretches for over 10 miles across ...
... 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 Ghurghushti plain stretches for over 10 miles across ...
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