Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 1
1 - 26 THE GEOLOGY OF THE ATTOCK - CHERAT RANGE , WEST PAKISTAN R
. A . KHAN TAHIRKHELI ABSTRACT The Attock - Cherat Range is exposed in an
area of about 50 square miles in Attock district and 360 square miles in the ...
1 - 26 THE GEOLOGY OF THE ATTOCK - CHERAT RANGE , WEST PAKISTAN R
. A . KHAN TAHIRKHELI ABSTRACT The Attock - Cherat Range is exposed in an
area of about 50 square miles in Attock district and 360 square miles in the ...
Page 3
Between Attock and Mir Kalan – a hamlet located on the eastern fringe of the
Cherat peak , the general trend of the range is parallel to the east - west strike
and corresponds with the main structural line of the area . Beyond Mir Kalan , the
...
Between Attock and Mir Kalan – a hamlet located on the eastern fringe of the
Cherat peak , the general trend of the range is parallel to the east - west strike
and corresponds with the main structural line of the area . Beyond Mir Kalan , the
...
Page 23
The pelite of the Attock - Cherat Range , which was previously considered to be
undifferentiated , has been divided into two parts , the Manki Slate and the Attock
Shale ; the former is placed in the Lower to Middle Silurian and the latter has ...
The pelite of the Attock - Cherat Range , which was previously considered to be
undifferentiated , has been divided into two parts , the Manki Slate and the Attock
Shale ; the former is placed in the Lower to Middle Silurian and the latter has ...
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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