Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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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
Thus the constituents of the Jutana Dolomite, at the time of deposition, were in
granular form, indicating transportation. While there can be no question about the
granular nature of the constituents of the Baghanwala Formation. The presence
of ...
Thus the constituents of the Jutana Dolomite, at the time of deposition, were in
granular form, indicating transportation. While there can be no question about the
granular nature of the constituents of the Baghanwala Formation. The presence
of ...
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Contents
and the Baghanwala Formation | 1 |
Khewra Gorge Khewra Jehlutn District | 11 |
Mineral Poliey with special reference | 41 |
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Common terms and phrases
anhedral Baghanwala Formation basal basin biotite calcarenite calcareous cement calcilutite texture calcisiltite texture calcite Cambrian carbonate and limonite carbonate matrix carbonate minerals Cementing material characterized by calcarenite chlorite clayey cement colour Compactibility corroded boundaries cross-bedding cubic pseudomorphs deposition detrital Dolomitic limestone environments feldspar fossils freely circulated Geology of India Ghundai Sar glauconite granoblastic highly corroded indicate interbeddings intercalations iron oxide iron oxide pigmentation Jehlum KHAN Khewra Gorge Khussak Formation Khyber Agency laminated layers less corroded long shore currents marine water maroon material is carbonate metamorphism mica micaceous mineral sector Minerals are anhedral mud cracks Muscovite non-clastic observed Pakistan Peshawar PETROGRAPHY Plagioclase porosity pseudomorphs Punjab quartz quartz grains recrystallized ripple marks rock texture salt crystals Salt Range sandstone sedimentary rocks sedimentary structures sediments shale siltstone slides stable shelf area strata stratification stratigraphic stratigraphic levels stylolites texture is metamorphic thin bedded Thin Section Tobra Formation underlying Jutana Dolomite Univ upper worm burrows