Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 1
... RANGE , WEST PAKISTAN R. A. KHAN TAHIRKHELI ABSTRACT The Attock - Cherat Range is exposed in an area of about 50 square miles in Attock district and 360 square miles in the Peshawar district , on both the sides of the Indus River ...
... RANGE , WEST PAKISTAN R. A. KHAN TAHIRKHELI ABSTRACT The Attock - Cherat Range is exposed in an area of about 50 square miles in Attock district and 360 square miles in the Peshawar district , on both the sides of the Indus River ...
Page 3
... range is parallel to the east - west strike and corresponds with the main structural line of the area . Beyond Mir Kalan , the Cherat Range swings to the northeast , involving the strike and the main structural features of the area ...
... range is parallel to the east - west strike and corresponds with the main structural line of the area . Beyond Mir Kalan , the Cherat Range swings to the northeast , involving the strike and the main structural features of the area ...
Page 21
... range . The rocks generally dip to the north at angles varying between 25 and 70 degrees . Along the southern front of the range , the dips are comparatively steeper . The predominant east - west strike gives way to northeast ...
... range . The rocks generally dip to the north at angles varying between 25 and 70 degrees . Along the southern front of the range , the dips are comparatively steeper . The predominant east - west strike gives way to northeast ...
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