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
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 . Alternating layers of shales were
deposited .
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 . Alternating layers of shales were
deposited .
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
1979 No | 1 |
Khewra Gorge Khewra Jehluu District | 11 |
Khewra Gorge Khewra Jehlum District | 21 |
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Common terms and phrases
abundant anhedral appears Baghanwala Formation basal base basin biotite brown Bull calcarenite calcareous calcareous cement calcite Cambrian carbonate carbonate and limonite carbonate minerals Cementing material characterized chlorite circulated clastic clay clear colour common Compactibility constituents contains corroded boundaries crystals cubic currents deposition dominant Early effects environments exposed field formed fossils Geol Geology glauconite important India indicate industries interbeddings intercalations iron oxide Jutana Dolomite KHAN Khewra Gorge laminated layers less limestone limonite maroon material is carbonate matrix medium metamorphism meters mica micaceous minerals noticed observed occurs olive origin Pakistan Peshawar pigmentation places porosity present primary pseudomorphs Punjab quartz grains recrystallized result ripple marks rocks rounded Saline Salt Range sand sandstone sector sedimentary sediments seen shale shallow slides solution strata stratification structures stylolites suggestive texture thick thin bedded Thin Section tion underlying Univ upper various vary warm writers York