Geological Bulletin, Volume 14University of Peshawar, 1981 - Geology |
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Page 71
In most of the sections , these cherty zones are overlain by thick bedded to
massive beds of dolomite . Overlaying this dolomite is a thick sequence of
dolomitic limestone and at about 90 to 110 m the section changes from thick
bedded ...
In most of the sections , these cherty zones are overlain by thick bedded to
massive beds of dolomite . Overlaying this dolomite is a thick sequence of
dolomitic limestone and at about 90 to 110 m the section changes from thick
bedded ...
Page 125
Biotite Granite Gneiss In Mauji , gneissic rocks are exposed in a body about 150
metres thick following the trend of foliation of the ... Southwards , in Reshian the
gneiss attains a thickness of about 450 m and extends NW to Mauji ( Fig . 2 ) .
Biotite Granite Gneiss In Mauji , gneissic rocks are exposed in a body about 150
metres thick following the trend of foliation of the ... Southwards , in Reshian the
gneiss attains a thickness of about 450 m and extends NW to Mauji ( Fig . 2 ) .
Page 193
In this zone the Jurassics are mainly comprised of thick to thin bedded limestone
inter - bedded with shales . In the allochthonous zone , such as the Ziarat -
Harnai region , an undisturbed thick succession ( 133 in plus ) of Jurassic strata ...
In this zone the Jurassics are mainly comprised of thick to thin bedded limestone
inter - bedded with shales . In the allochthonous zone , such as the Ziarat -
Harnai region , an undisturbed thick succession ( 133 in plus ) of Jurassic strata ...
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Contents
The Geology and Petrography of the Tarbela Alkaline Complex | 1 |
Petrography of the Loe Shilman Carbonatite Complex Khyber Agency | 29 |
Major Elements Abundance in the Kalam Lavas | 45 |
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Common terms and phrases
abundant albite albitites alkaline altered amphibole andesite apatite associated band basic beds belt biotite bodies brown Bull calcite carbonate carbonatite chemical chlorite complex composition consist contain deposits described detailed developed diorites dolomite epidote et al fault feldspar field Formation gabbroic Geol Geology gneisses grains granites granitic rocks green Himalayas hornblende igneous indicate Indus intrusions island arc Jurassic Kalam Karakoram Kempe Kohistan Late Limestone locally lower magmatic magnetite major margin metamorphism microfacies minerals minor muscovite normal northern obducted occur origin outcrop Pakistan Peshawar petrography phases plagioclase Plate Pleistocene present pyrite pyrochlore quartz quartzite range region reported river rocks samples sandstones schists sediments sequence sericite shales similar Siwalik sphene structure suggest Swat syenites Table Tahirkheli Tarbela tectonic thick thin Traces Univ University Upper Valley varieties veins volcanic Warsak West zone