Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 13
The unit comprises three lithologies ; limestone is dominant , with soubrodinate
quartzite and shale . It overlies the Khattak Limestone with a well marked
unconformity . The bottom bed is composed of quartzite and quartzitic sandstone
which ...
The unit comprises three lithologies ; limestone is dominant , with soubrodinate
quartzite and shale . It overlies the Khattak Limestone with a well marked
unconformity . The bottom bed is composed of quartzite and quartzitic sandstone
which ...
Page 113
This is the dominant species . Locality : Lumshiwal Nala , Surghar Range .
CINCORIOLA SP . A SP . NOV . ( PLATE 1 , FIG . 2 ) Material : Three fairly well -
preserved specimens . Horizon : Eight inches thick , dark gray limestone bed , a
foot ...
This is the dominant species . Locality : Lumshiwal Nala , Surghar Range .
CINCORIOLA SP . A SP . NOV . ( PLATE 1 , FIG . 2 ) Material : Three fairly well -
preserved specimens . Horizon : Eight inches thick , dark gray limestone bed , a
foot ...
Page 117
... Dadu , and Mullagori are the dominant tribes inhabiting the area . Besides
agriculture and transit trade , marble excavation and soapstone mining are the
main mineral supported professions within the area . PREVIOUS WORK Prior to
1965 ...
... Dadu , and Mullagori are the dominant tribes inhabiting the area . Besides
agriculture and transit trade , marble excavation and soapstone mining are the
main mineral supported professions within the area . PREVIOUS WORK Prior to
1965 ...
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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