Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 31
be gneissose , and strike parallel to the general east - west trend of the
Hornblendic Group which , apparently , surrounds the schists on all sides . At
many places , the Hornblendic Group crops out within the schists , indicating the
intrusive ...
be gneissose , and strike parallel to the general east - west trend of the
Hornblendic Group which , apparently , surrounds the schists on all sides . At
many places , the Hornblendic Group crops out within the schists , indicating the
intrusive ...
Page 70
... of Baltoro ) | Karakoram Granodiorite III Kristallinschiefer ( Older schists and
gneisses ) Zentral Kristallin ( Palaeozoic metamorphics and younger Variscan
granites ) ( C ) Central Schist - gneiss zone ( Mica - schists and gneissesderived
from ...
... of Baltoro ) | Karakoram Granodiorite III Kristallinschiefer ( Older schists and
gneisses ) Zentral Kristallin ( Palaeozoic metamorphics and younger Variscan
granites ) ( C ) Central Schist - gneiss zone ( Mica - schists and gneissesderived
from ...
Page 106
Phyllitic Schists 3 . Marble and Calcareous Schists 2 . Amphibolite Horizon 1 .
Siliceous Schists Jan and Tahirkheli ( 1969 ) , however , have not extended this
subdivision in the lower part of Indus Kohistan of Swat . According to these
workers ...
Phyllitic Schists 3 . Marble and Calcareous Schists 2 . Amphibolite Horizon 1 .
Siliceous Schists Jan and Tahirkheli ( 1969 ) , however , have not extended this
subdivision in the lower part of Indus Kohistan of Swat . According to these
workers ...
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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