Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 6
This belt is developed along the northern face of the Attock - Cherat Range
running parallel to , and apparently dipping under the Nowshera reef outcrops .
These rocks may be correlated on lithological basis with the similar rock outcrops
in ...
This belt is developed along the northern face of the Attock - Cherat Range
running parallel to , and apparently dipping under the Nowshera reef outcrops .
These rocks may be correlated on lithological basis with the similar rock outcrops
in ...
Page 29
( 1962 ) gave this name to the hornblende - rich rocks occupying a wide belt of
country in the Upper Swat . The group was considered to be thrust over the
younger ( Siluro - Devonian ) rocks of the Lower Swat - Buner Schistose Group
which ...
( 1962 ) gave this name to the hornblende - rich rocks occupying a wide belt of
country in the Upper Swat . The group was considered to be thrust over the
younger ( Siluro - Devonian ) rocks of the Lower Swat - Buner Schistose Group
which ...
Page 98
The rocks of the Upper Swat , probably , are a southwestwards continuation of
the Himalayas west of the Balakot syntaxis . Hayden ( 1915 ) thinks that the belt
of igneous and metamorphic rocks running through the outer mountains of Dir
and ...
The rocks of the Upper Swat , probably , are a southwestwards continuation of
the Himalayas west of the Balakot syntaxis . Hayden ( 1915 ) thinks that the belt
of igneous and metamorphic rocks running through the outer mountains of Dir
and ...
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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