Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 5
... probably high energy environments must have prevailed during the deposition of atleast a portion of the Baghanwala Formation . A block from the Jutana Dolimite indicated that large ripple marks were formed at first which were ...
... probably high energy environments must have prevailed during the deposition of atleast a portion of the Baghanwala Formation . A block from the Jutana Dolimite indicated that large ripple marks were formed at first which were ...
Page 29
... probably , terristerial conditions of non- deposition prevailed for a long stretch of time . The area recorded heavy and extensive glaciation during Early Permian times , the record of this glaciation is preserved in the form of the ...
... probably , terristerial conditions of non- deposition prevailed for a long stretch of time . The area recorded heavy and extensive glaciation during Early Permian times , the record of this glaciation is preserved in the form of the ...
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