Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 35
Cementing material is carbonate. Coiumnals of crinoids, Cladopora, and
Favosiits are in the fragmental form. Environment of deposition is clear, warm,
shallow and freely circulated water in the stable shelf area. Thin Section No. 15—
17.
Cementing material is carbonate. Coiumnals of crinoids, Cladopora, and
Favosiits are in the fragmental form. Environment of deposition is clear, warm,
shallow and freely circulated water in the stable shelf area. Thin Section No. 15—
17.
Page 36
Cementing material is carbonate and limonite. Fossils are indistinctive and
completely recrystallized due to the dolomitization mainly, and metamorphism
secondarily. This section suggests conditions of shallow, warm, clear and free
circulated ...
Cementing material is carbonate and limonite. Fossils are indistinctive and
completely recrystallized due to the dolomitization mainly, and metamorphism
secondarily. This section suggests conditions of shallow, warm, clear and free
circulated ...
Page 37
Cementing materials are carbonate, limonite, and quartz. Fossils are highly
recrystallized and indistinctive. Non-clastic material deposited from the shallow,
clear, and free circulated warm marine water while igneous material in the
particular ...
Cementing materials are carbonate, limonite, and quartz. Fossils are highly
recrystallized and indistinctive. Non-clastic material deposited from the shallow,
clear, and free circulated warm marine water while igneous material in the
particular ...
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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