Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 26
baDk do not extend on the eastern side which is occupied by diorites of different
appearance and texture. It can thus be assumed that a fault runs along the
stream to the south of Dewangar. Consequently, the western part of the valley
having ...
baDk do not extend on the eastern side which is occupied by diorites of different
appearance and texture. It can thus be assumed that a fault runs along the
stream to the south of Dewangar. Consequently, the western part of the valley
having ...
Page 35
The eastern drainage is captured by Dor and Haro rivers through numerous
seasonal khwars which ultimately carry the water to Indus. The Gandghar Range
varies in elevations from less than 1,500 feet near the extreme ends, the north
and ...
The eastern drainage is captured by Dor and Haro rivers through numerous
seasonal khwars which ultimately carry the water to Indus. The Gandghar Range
varies in elevations from less than 1,500 feet near the extreme ends, the north
and ...
Page 36
This limestone is exposed in three isolated sections; two located on the western
fringe and another along the eastern foothill of the Gandghar Range. The type
section of this limestone is exposed near Mohat Nawan village, located about
half a ...
This limestone is exposed in three isolated sections; two located on the western
fringe and another along the eastern foothill of the Gandghar Range. The type
section of this limestone is exposed near Mohat Nawan village, located about
half a ...
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Contents
Preliminary geology and petrography of Swat Kohistan | 1 |
No 1 December | 3 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
8 other sections not shown
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Common terms and phrases
abundant acid amphibolites associated Bajaur bands beds biotite brines Bull calcite carbonates chloride complexes chlorite coarse-grained colour concentration correlated crystals dark deposits Deshai developed Dewangar diorites dolerite dolomite dykes east eastern epidote exposed extend feet thick feldspar fluid inclusions folded foliation fractures Gabral Gandghar Range garnet Geol geology glauconite gneisses gneissose grades grains granites graphite grey Hazara hornblende hornblendites hydrothermal solutions hypersthene igneous ilmenite Indus intrusions Kalam Group Khan Khussak Formation Kohistan layers limestone locally magma magnetite marble Matiltan Matsushita metals metamorphism miles mineralizing solutions Misri Banda Quartzite norites Nowshera occur outcrop Pakistan pegmatite pegmatite veins peridotite Peshawar phenocrysts phyllites plagioclase plutonic porphyritic pyrite pyroxene pyroxenites quartz quartzite region samples sandstone schists sediments sericite shale sheared Sirikot Sirikot Slates solubility sphalerite sphene sulphide sulphur Surv Swat Kohistan Tahirkheli temperature Tertiary thin transport Univ Upper Swat Ushu usually Utror valley volcanic rocks waters well-developed zone