Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 22
Presence of these structures combined with the mineralogical composition
indicate that during the deposition of the Baghanwala Formation, salinity of the
basin was high which resulted in the crystallization of salt crystals. However, the
salt ...
Presence of these structures combined with the mineralogical composition
indicate that during the deposition of the Baghanwala Formation, salinity of the
basin was high which resulted in the crystallization of salt crystals. However, the
salt ...
Page 23
Fucoid markings are reported by many others. The primary sedimentary
structures noticed in this formation ate indicative of deposition in shallow water
environments. The salinity of water in the basin was too high, and the depth was
shallow.
Fucoid markings are reported by many others. The primary sedimentary
structures noticed in this formation ate indicative of deposition in shallow water
environments. The salinity of water in the basin was too high, and the depth was
shallow.
Page 24
minerals took place in the basin containing terrigenous quartz grains. The
abundance of the carbonate matrix is the result of same process. The other
explanation which can be forwarded is that the carbonate flowed into the basin
alongwith ...
minerals took place in the basin containing terrigenous quartz grains. The
abundance of the carbonate matrix is the result of same process. The other
explanation which can be forwarded is that the carbonate flowed into the basin
alongwith ...
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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