Geological Bulletin, Volume 5University of Peshawar - Geology |
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Page 17
... feet , whereas , in the latter section , which was measured by Meissner and Master ( 1959-60 unpublished ) , it has a thickness of 140 feet . It consists of sandstone , shale , loose and soft clay ; purple to yellowish brown , dull red ...
... feet , whereas , in the latter section , which was measured by Meissner and Master ( 1959-60 unpublished ) , it has a thickness of 140 feet . It consists of sandstone , shale , loose and soft clay ; purple to yellowish brown , dull red ...
Page 90
... feet in thickness is recognized as the Misri Banda Quartzite . ( v ) The Warran Ghundai Formation , about 1,200 feet thick , is both lithologically and palaeontologically different from other forma- tions exposed in the area . It ...
... feet in thickness is recognized as the Misri Banda Quartzite . ( v ) The Warran Ghundai Formation , about 1,200 feet thick , is both lithologically and palaeontologically different from other forma- tions exposed in the area . It ...
Page 124
... feet ) and overlain by medium - grained quartzites ( 60 feet ) , was named by Stauffer ( 1967 , p . 548 ) after the village of Ali Masjid ( lat . 34 ° 02 ′ N , long . 71 ° 15 ' E ) . The formation is well exposed in the investigated ...
... feet ) and overlain by medium - grained quartzites ( 60 feet ) , was named by Stauffer ( 1967 , p . 548 ) after the village of Ali Masjid ( lat . 34 ° 02 ′ N , long . 71 ° 15 ' E ) . The formation is well exposed in the investigated ...
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