Geological Bulletin, Volume 14University of Peshawar, 1981 - Geology |
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Page 164
However , in view of the current thoughts on granites , the gradually diminishing
support for the hypothesis of large - scale granitization , and the information
provided by Le Fort et al . ( 1980 ) for the Mansehra pluton , we would favour a
partial ...
However , in view of the current thoughts on granites , the gradually diminishing
support for the hypothesis of large - scale granitization , and the information
provided by Le Fort et al . ( 1980 ) for the Mansehra pluton , we would favour a
partial ...
Page 197
A thick succession of strongly current - bedded massive oolitic limestone during
the Middle Jurassic suggests shallowing of the Tethys and deposition under
conditions of greater disturbance and agitation and probably a warmer climate .
A thick succession of strongly current - bedded massive oolitic limestone during
the Middle Jurassic suggests shallowing of the Tethys and deposition under
conditions of greater disturbance and agitation and probably a warmer climate .
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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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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