Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 3
... constituents , indi- cated by thin strata , may be the result of the difference in the grain size , roundness , and sphericity of the clastic particles . CROSS BEDDING Cross bedding is the internal structure preserved in the strata ...
... constituents , indi- cated by thin strata , may be the result of the difference in the grain size , roundness , and sphericity of the clastic particles . CROSS BEDDING Cross bedding is the internal structure preserved in the strata ...
Page 5
... 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 ...
... 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 ...
Page 15
... constituents , and rest as the matrix . Exclud- ing the slide No. 4 and 8 the maximum percentage of the carbonate ... constituent of the Baghanwala Forma- tion , and is more prominant in the upper part than the basal part . Biotite ...
... constituents , and rest as the matrix . Exclud- ing the slide No. 4 and 8 the maximum percentage of the carbonate ... constituent of the Baghanwala Forma- tion , and is more prominant in the upper part than the basal part . Biotite ...
Contents
and the Baghanwala Formation | 1 |
Khewra Gorge Khewra Jehlum District | 11 |
Khewra Gorge Khewra Jehlum District | 21 |
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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 clastic clayey cement colour Compactibility corroded boundaries cross-bedding cubic pseudomorphs deposition detrital Dolomitic limestone environments feldspar fossils freely circulated Geology of India glauconite Grains are subrounded granoblastic highly corroded indicate interbeddings intercalations iron oxide iron oxide pigmentation Jehlum KHAN Khewra Gorge Khyber Agency laminated layers less corroded limestone long shore currents marine water maroon material is carbonate metamorphism meters mica micaceous mineral sector Minerals are anhedral mud cracks 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 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