Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 3
... outcrops extend into the Peshawar Plain without any interruption , and culminate to 4546 and 5033 feet elevations at ... outcrops of the Triassic to Pleistocene age . The Cherat Range forms a steep escarpment over- looking Nizampur and ...
... outcrops extend into the Peshawar Plain without any interruption , and culminate to 4546 and 5033 feet elevations at ... outcrops of the Triassic to Pleistocene age . The Cherat Range forms a steep escarpment over- looking Nizampur and ...
Page 14
... outcrop extends to the eastern bank of the Indus and the prominent Dakhner Fort , now abandoned , is built over this ... outcrops are located about one and half mile west of Anzari village , and at Amiru village . Between Mir Kalan and ...
... outcrop extends to the eastern bank of the Indus and the prominent Dakhner Fort , now abandoned , is built over this ... outcrops are located about one and half mile west of Anzari village , and at Amiru village . Between Mir Kalan and ...
Page 15
... outcrops south of Manki , the siltstone forms conspicuous bands in the Attock Shale . The bands range in thickness from 2 to 10 feet and predomi- nate in most of the sections . In the eastern outcrop the silty part of the formation ...
... outcrops south of Manki , the siltstone forms conspicuous bands in the Attock Shale . The bands range in thickness from 2 to 10 feet and predomi- nate in most of the sections . In the eastern outcrop the silty part of the formation ...
Contents
Vol | 1 |
Vol | 5 |
Petrography of the upper part of Kohistan and southwestern Gilgit | 27 |
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Common terms and phrases
abundant Ahmad Ali Masjid altered amphibole amphibolites Attock Attock Slates Attock-Cherat Range bands biotite Bull calcareous calcite carbonate Carboniferous Cherat chlorite colour correlated Cretaceous cross-bedding Darwazai deposits Devonian diorites dolomite epidote exposed feet thick feldspar fossils fractures garnet Geol geology Gilgit Agency gneisses grains granitic green grey Hazara District hornblende Ibid igneous India Indus River intrusions Jamrud Jan and Tahirkheli Jour Khan Khattak Khewra Formation Khwar Khyber Agency Kohat Kohistan Landikotal Slate limestone lithological Manki Slate Masjid Formation metamorphism metasedimentary miles minerals minor Mohmand Agency muscovite nala norites Nowshera occur outcrops Palaeozoic Paleocene Panjab Univ pegmatites Peshawar phyllites plagioclase pyroxene quartz quartzite reef region Rehman Ripple Marks rocks Salt Range sandstone Schistose Group schists sedimentary Shagai Shagai Limestone Shah Dheri shale Silurian Siluro-Devonian slaty shale Stauffer stratigraphic structures Surv Tertiary thin bedded Thin Section ultramafic veins weathered West Pakistan yellowish