Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 1
In the two formations , several primary , secondary and organic structures are
well preserved . In this paper the writer has described some of the most
interesting and conspicuous primary , secondary and organic structures well
preserved in ...
In the two formations , several primary , secondary and organic structures are
well preserved . In this paper the writer has described some of the most
interesting and conspicuous primary , secondary and organic structures well
preserved in ...
Page 23
Other primary sedimentary structures observed are ripple marks , pseudomorphs
after salt crystals , fossil mud cracks , and worm burrows ( organic sedimentary
structures ) . Fucoid markings are reported by many others . The primary ...
Other primary sedimentary structures observed are ripple marks , pseudomorphs
after salt crystals , fossil mud cracks , and worm burrows ( organic sedimentary
structures ) . Fucoid markings are reported by many others . The primary ...
Page 29
CONCLUSION The Baghanwala Formation conformably overlics the Jutana
Dolomite and is composed of variegated shales with flaggy sandstone
interbeddings , Dark maroon colour and primary sedimentary features like ripple
marks , forsil ...
CONCLUSION The Baghanwala Formation conformably overlics the Jutana
Dolomite and is composed of variegated shales with flaggy sandstone
interbeddings , Dark maroon colour and primary sedimentary features like ripple
marks , forsil ...
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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