Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
From inside the book
Results 1-3 of 20
Page 1
The two formations represent deposition during Early to Middle Cambrian and in
fact form a part of a megacycle which started with the deposition of the Salt
Range Formation under arid and well oxygenated environment and culminated
with ...
The two formations represent deposition during Early to Middle Cambrian and in
fact form a part of a megacycle which started with the deposition of the Salt
Range Formation under arid and well oxygenated environment and culminated
with ...
Page 3
Overall mode of stratification suggests slight variation in the condition of
deposition . However , much arenaceous and argillaceous material was brought
into the basin of deposition during the time when lower part of the Jutana
Dolomite was ...
Overall mode of stratification suggests slight variation in the condition of
deposition . However , much arenaceous and argillaceous material was brought
into the basin of deposition during the time when lower part of the Jutana
Dolomite was ...
Page 5
Moreover , . . . " they indicate standing water at the time the ripples were formed "
( Dunbar and Rodgers , 1966 , p . 189 ) . Thus the constituents of the Jutana
Dolomite , at the time of deposition , were in granular form , indicating
transportation .
Moreover , . . . " they indicate standing water at the time the ripples were formed "
( Dunbar and Rodgers , 1966 , p . 189 ) . Thus the constituents of the Jutana
Dolomite , at the time of deposition , were in granular form , indicating
transportation .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
1979 No | 1 |
Khewra Gorge Khewra Jehluu District | 11 |
Khewra Gorge Khewra Jehlum District | 21 |
1 other sections not shown
Other editions - View all
Common terms and phrases
abundant anhedral appears Baghanwala Formation basal base basin biotite brown Bull calcarenite calcareous calcareous cement calcite Cambrian carbonate carbonate and limonite carbonate minerals Cementing material characterized chlorite circulated clastic clay clear colour common Compactibility constituents contains corroded boundaries crystals cubic currents deposition dominant Early effects environments exposed field formed fossils Geol Geology glauconite important India indicate industries interbeddings intercalations iron oxide Jutana Dolomite KHAN Khewra Gorge laminated layers less limestone limonite maroon material is carbonate matrix medium metamorphism meters mica micaceous minerals noticed observed occurs olive origin Pakistan Peshawar pigmentation places porosity present primary pseudomorphs Punjab quartz grains recrystallized result ripple marks rocks rounded Saline Salt Range sand sandstone sector sedimentary sediments seen shale shallow slides solution strata stratification structures stylolites suggestive texture thick thin bedded Thin Section tion underlying Univ upper various vary warm writers York