Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 3
West of the river , the outcrops extend into the Peshawar Plain without any
interruption , and culminate to 4546 and 5033 feet elevations at Cherat and
Jalala Sar respectively . These two peaks form commanding heights overlooking
the ...
West of the river , the outcrops extend into the Peshawar Plain without any
interruption , and culminate to 4546 and 5033 feet elevations at Cherat and
Jalala Sar respectively . These two peaks form commanding heights overlooking
the ...
Page 14
This outcrop extends to the eastern bank of the Indus and the prominent Dakhner
Fort , now abandoned , is built over this . ... Further west , two isolated outcrops
are located about one and half mile west of Anzari village , and at Amiru village .
This outcrop extends to the eastern bank of the Indus and the prominent Dakhner
Fort , now abandoned , is built over this . ... Further west , two isolated outcrops
are located about one and half mile west of Anzari village , and at Amiru village .
Page 15
In the outcrops west of the Indus River , the Attock Shale spreads for over six
miles across the Chcrat ridge , forming thick monotonous sequence of shale and
slaty shale with intercalated siltstone . A yellowish brown concretionary limestone
is ...
In the outcrops west of the Indus River , the Attock Shale spreads for over six
miles across the Chcrat ridge , forming thick monotonous sequence of shale and
slaty shale with intercalated siltstone . A yellowish brown concretionary limestone
is ...
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Common terms and phrases
abundant Agency Ahmad altered amphibolites appears associated Attock Slates Attock-Cherat bands base basis brown Bull Cherat chlorite clay colour common composed composition considered contains correlated Cretaceous Davies deposits detailed developed diorites District east epidote exposed extends feet feldspar Formation fossils fractures garnet Geol geology Gilgit gneisses grains granitic green grey Hazara Hornblendic Group Ibid India Indus intrusions iron Jour Khan Khyber latter light limestone Long Lower mainly major Manki Marks Martin Masjid material metamorphic Middle miles minerals minor norites northern occur outcrops Panjab Peshawar Phyllite places plagioclase present probably quartz quartzite Range reef region reported River rocks samples sandstone Schistose schists sericite Shah shale shows Silurian southern Stauffer stratigraphic structure suggests Surv Swat Tahirkheli thick thin Thin Section units Univ Upper Valley various veins village weathered West Pakistan western