Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 20
Cherat Range . They are not found in the Mesozoic and Tertiary rock formations ,
which is suggestive of the fact that their age is pre - Mesozoic . The sills are
yellowish brown , medium - to fine - grained and are concordant to the structure .
Cherat Range . They are not found in the Mesozoic and Tertiary rock formations ,
which is suggestive of the fact that their age is pre - Mesozoic . The sills are
yellowish brown , medium - to fine - grained and are concordant to the structure .
Page 92
The alternation of limestones , quartzites , and graphitic schists is suggestive of
cyclic sedimentation occasionally in swampy and lagoonal environments ( as
indicated by the presence of graphitic schists - the metamorphic ...
The alternation of limestones , quartzites , and graphitic schists is suggestive of
cyclic sedimentation occasionally in swampy and lagoonal environments ( as
indicated by the presence of graphitic schists - the metamorphic ...
Page 121
The gouging of slates , and shearing and brecciation of the quartzites is
suggestive of a thrust contact . Age and Correlation . In a regional correlation
scheme , Stauffer ( 1967 ) correlated the Landikotal Slate with the Kandar Phyllite
of ...
The gouging of slates , and shearing and brecciation of the quartzites is
suggestive of a thrust contact . Age and Correlation . In a regional correlation
scheme , Stauffer ( 1967 ) correlated the Landikotal Slate with the Kandar Phyllite
of ...
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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