Geological Bulletin, Volume 5University of Peshawar - Geology |
From inside the book
Results 1-3 of 9
Page 55
... different kinds of ripple marks have been identified : ( a ) Oscillation Ripple
Marks ( b ) Wave and Current Ripple Marks ... identified uptil now , may be
present in this formation as the swiftly changing currents and the deposition in the
shallow ...
... different kinds of ripple marks have been identified : ( a ) Oscillation Ripple
Marks ( b ) Wave and Current Ripple Marks ... identified uptil now , may be
present in this formation as the swiftly changing currents and the deposition in the
shallow ...
Page 60
5) suggets currents of too low intensity to drive or overturn the grain so that
precipitation of CaCOj continued only on one side. Sparry cement shows
washing phenomenon. Presence of articulated ostra- codes indicates optimum
conditions for ...
5) suggets currents of too low intensity to drive or overturn the grain so that
precipitation of CaCOj continued only on one side. Sparry cement shows
washing phenomenon. Presence of articulated ostra- codes indicates optimum
conditions for ...
Page 60
5 ) suggets currents of too low intensity to drive or overturn the grain so that
precipitation of CaCO3 continued only on one side . Sparry cement shows
washing phenomenon . Presence of articulated ostra . codes indicates optimum
conditions ...
5 ) suggets currents of too low intensity to drive or overturn the grain so that
precipitation of CaCO3 continued only on one side . Sparry cement shows
washing phenomenon . Presence of articulated ostra . codes indicates optimum
conditions ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Other editions - View all
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