Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 7
Cubic pseudomorphs after salt crystals are abundantly present in the
Baghanwala Formation . It is because of their abundance that the formation was
formerly called " Salt Pseudomorph Beds ” . The size of the cubic pseduomorphs
after salt ...
Cubic pseudomorphs after salt crystals are abundantly present in the
Baghanwala Formation . It is because of their abundance that the formation was
formerly called " Salt Pseudomorph Beds ” . The size of the cubic pseduomorphs
after salt ...
Page 22
Oxidation effects are also pronounced and at some places pseudomorphs of
biotite are recognized . Primary sedimentary structures noticed are stratification ,
cross - bedding , ripple marks , worm burrows , and cubic pseudomorphs of balite
.
Oxidation effects are also pronounced and at some places pseudomorphs of
biotite are recognized . Primary sedimentary structures noticed are stratification ,
cross - bedding , ripple marks , worm burrows , and cubic pseudomorphs of balite
.
Page 27
cement Micaceous sandstone , brown , fine grained , thin bedded , intercalations
of shale , cubic pseudomorphs abundant , micaceous minerals prominent ,
abundant iron oxide pigmentation , loosely gemented , calcareous and clayey
cement ...
cement Micaceous sandstone , brown , fine grained , thin bedded , intercalations
of shale , cubic pseudomorphs abundant , micaceous minerals prominent ,
abundant iron oxide pigmentation , loosely gemented , calcareous and clayey
cement ...
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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