Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 65
The rocks of the Landikotal area , Khyber Agency , have been divided into three
major parts by Stauffer ( in review ) . Two of them , i . e . the lower Landikital Slate
and the upper Shahgai Limestone - including coralline limestones — have been
...
The rocks of the Landikotal area , Khyber Agency , have been divided into three
major parts by Stauffer ( in review ) . Two of them , i . e . the lower Landikital Slate
and the upper Shahgai Limestone - including coralline limestones — have been
...
Page 91
As Stauffer ' s investigations were limited only along the Khyber Pass , he could
not record the lithological heterogeneity of the Ali Masjid “ Formation ” . During
1968 , 1969 , and 1970 , the writer had numerous opportunities to visit the Khyber
...
As Stauffer ' s investigations were limited only along the Khyber Pass , he could
not record the lithological heterogeneity of the Ali Masjid “ Formation ” . During
1968 , 1969 , and 1970 , the writer had numerous opportunities to visit the Khyber
...
Page 92
... and palaeontological simlarities , the names Kandar Phyllite , Nowshera
Formation , and Misri Banda Quartzite , as proposed by Stauffer ( 1968 ) , are
extended to Phyllite , reef carbonate and quartzite of Guddar - - Warran Ghundai
Section .
... and palaeontological simlarities , the names Kandar Phyllite , Nowshera
Formation , and Misri Banda Quartzite , as proposed by Stauffer ( 1968 ) , are
extended to Phyllite , reef carbonate and quartzite of Guddar - - Warran Ghundai
Section .
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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