Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 85
REHMAN , J . and ZEB , A . , 1970 — The geology of the Shah Dheri - Kabal area
, Swat . Geol . Bull . Univ . Peshawar , vol . 5 . * Rossi RONCHETTI , C . and
MIRELLI , A . F . , 1959 — Rudistids and nereids of north - west Pakistan
Cretaceous ...
REHMAN , J . and ZEB , A . , 1970 — The geology of the Shah Dheri - Kabal area
, Swat . Geol . Bull . Univ . Peshawar , vol . 5 . * Rossi RONCHETTI , C . and
MIRELLI , A . F . , 1959 — Rudistids and nereids of north - west Pakistan
Cretaceous ...
Page 108
The corundum - bearing rocks are at two places ; one , about a mile and a half
southwest , and the other , about two miles north of Shah Dheri . In the former
locality , the mineral occurs in a greenish , massive body that is bordered by
banded ...
The corundum - bearing rocks are at two places ; one , about a mile and a half
southwest , and the other , about two miles north of Shah Dheri . In the former
locality , the mineral occurs in a greenish , massive body that is bordered by
banded ...
Page 119
CCU Ibrahim Shah ( 1969 ) practically follows the same pattern as put forward by
Stauffer . He reported a number of index fossils from Khyber Agency dur
investigations . A detailed report , being prepared by John A . Talent , on the
taxonomy ...
CCU Ibrahim Shah ( 1969 ) practically follows the same pattern as put forward by
Stauffer . He reported a number of index fossils from Khyber Agency dur
investigations . A detailed report , being prepared by John A . Talent , on the
taxonomy ...
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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