Geological Bulletin, Volume 11University of Peshawar, 1979 - Geology |
From inside the book
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Page 10
... east - west extension , the eastern limit being Ushu Valley and in the west they traverse the northwestern part of Dir district and cross the Afghanistan border in Bajaur . Their maximum thickness estimated to be 1000-1200 meters has ...
... east - west extension , the eastern limit being Ushu Valley and in the west they traverse the northwestern part of Dir district and cross the Afghanistan border in Bajaur . Their maximum thickness estimated to be 1000-1200 meters has ...
Page 8
... east - west extension , the eastern limit being Ushu Valley and in the west they traverse the northwestern part of Dir district and cross the Afghanistan border in Bajaur . Their maximum thickness estimated to be 1000-1200 meters has ...
... east - west extension , the eastern limit being Ushu Valley and in the west they traverse the northwestern part of Dir district and cross the Afghanistan border in Bajaur . Their maximum thickness estimated to be 1000-1200 meters has ...
Page 26
... east of the Chitral border . The Ladakh Range is located in Baltistan and constitutes high ranges of Deosai plateau and Shyok Valley , south of Skardu . The eastern flank of the Nanga Parbat - Haramosh loop delimits the western boundary ...
... east of the Chitral border . The Ladakh Range is located in Baltistan and constitutes high ranges of Deosai plateau and Shyok Valley , south of Skardu . The eastern flank of the Nanga Parbat - Haramosh loop delimits the western boundary ...
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Common terms and phrases
abundant amphibole amphibolites andesite anorthosite assemblages associated Bajaur Baltistan bands Baraul belt biotite Bull calc-alkaline Chaudhry Chitral chlorite clinopyroxene coarse-grained composition contain Cretaceous Desio Diwangar epidote fault feldspar foliation Formation garnet granulites Geol Geology Gilgit gneisses gneissose grains granitic rocks Granodiorite granulites green Greenstone Complex grey Group Hazara Himalaya hornblende hypersthene igneous Indo-Pakistan Indus valley intrusions island arc Jan and Mian Jandul Kakar Kalam Karakoram Khan Kohistan layers limestone mafic magma Main Mantle Thrust margins metamorphic metasedimentary rocks metasediments mica Nanga Parbat norites occur opaque minerals orthopyroxene outcrops Pakistan pegmatites peridotites Peshawar Petrography petrology plagioclase plate pyroxene pyroxene granulites pyroxenites quartz diorites quartzites rarely region Reshun rutile schists sequence SiO2 slates southern sphene structure suture zone Swat Kohistan syntaxis Tahirkheli tectonic Tertiary texture thick trend tuffs twinning ultramafic rocks Univ Upper Swat Ushu Gol Utmankhel veins vicinity volcanic rocks whilst xenoliths Yasin