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 carbonate minerals are coarsely recrystallized in
the ghost structures , and merge into the fine grained calcareous matrix .
Recrystallization of the carbonate minerals is also an important textural feature
observed in a few slides . ... The carbonate minerals are coarsely recrystallized in
the ghost structures , and merge into the fine grained calcareous matrix .
Page 35
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 36
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 . Tbin
Section No .
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 . Tbin
Section No .
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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