Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 14
Recrystallization of the carbonate minerals is also an important textural feature
observed in a few slides. The process is, however, limited and appears to have
replaced some original pelletoid textural features. Thus only ghost structures are
...
Recrystallization of the carbonate minerals is also an important textural feature
observed in a few slides. The process is, however, limited and appears to have
replaced some original pelletoid textural features. Thus only ghost structures are
...
Page 36
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 water in the stable shelf area with
abundant ...
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 water in the stable shelf area with
abundant ...
Page 37
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 slide is present due to the intrusion. Thin Section No. 22.
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 slide is present due to the intrusion. Thin Section No. 22.
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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