Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 20
... magma . They are named by us as the Matiltan Granite . The last one , judging from the traverse of Matsushita ( 1965 , p . 45 ) along Dewangar Pass , may be of batholithic dimension and is named as the Dewangar Granite . The Matiltan ...
... magma . They are named by us as the Matiltan Granite . The last one , judging from the traverse of Matsushita ( 1965 , p . 45 ) along Dewangar Pass , may be of batholithic dimension and is named as the Dewangar Granite . The Matiltan ...
Page 23
... magma at depth . It may be the latter intrusions of the norite magma itself into the earlier , solidified norites , or of some other magma that has not been exposed yet by erosion , or 3 ) the joints may be due to the combination of the ...
... magma at depth . It may be the latter intrusions of the norite magma itself into the earlier , solidified norites , or of some other magma that has not been exposed yet by erosion , or 3 ) the joints may be due to the combination of the ...
Page 92
... magma , ( 2 ) assimilated , related to palingenic granitic magma of crustal origin , and ( 3 ) filtrational , related to the circulation of non magmatic uderground waters . The nature and Origin of Mineralizing Solutions . The various ...
... magma , ( 2 ) assimilated , related to palingenic granitic magma of crustal origin , and ( 3 ) filtrational , related to the circulation of non magmatic uderground waters . The nature and Origin of Mineralizing Solutions . The various ...
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