Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 36
... developed in a hillock in about two square miles area . Another section exposing this limestone occurs about two miles northeast of Ghazi village on the northern side of Kundi Darra . Its major outcrop is , however , exposed on the ...
... developed in a hillock in about two square miles area . Another section exposing this limestone occurs about two miles northeast of Ghazi village on the northern side of Kundi Darra . Its major outcrop is , however , exposed on the ...
Page 40
developed . However , in some areas located in the vicinity of Sirikot , Salam . khand , Chumyari and Thalikot villages , a few scattered and localized sections are recorded in the Sirikot slates which retain well - developed slaty ...
developed . However , in some areas located in the vicinity of Sirikot , Salam . khand , Chumyari and Thalikot villages , a few scattered and localized sections are recorded in the Sirikot slates which retain well - developed slaty ...
Page 79
... developed light grey shades . Beautiful yellowish - green shades have been developed duo to its close association with the ultramafic rocks to the north of Sheikh Ismail and Inzari Villages . The yellowish - green colour is imparted by ...
... developed light grey shades . Beautiful yellowish - green shades have been developed duo to its close association with the ultramafic rocks to the north of Sheikh Ismail and Inzari Villages . The yellowish - green colour is imparted by ...
Contents
Preliminary geology and petrography of Swat Kohistan | 1 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
Lithological classification and environment of deposition of | 43 |
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abundant altered amphibolites appears associated bands base beds biotite body brown Bull chlorite colour common complex concentration consist contain correlated cover crystalline crystals dark deposits developed diorites distance dykes east eastern epidote exposed extend feet feldspar folded foliation Formation fractures Gandghar Range garnet Geol geology gneisses grades grains granites green grey Group Hazara hornblende inches Indus intrusions iron Kalam Kohistan latter layers light limestone locally located Lower marble material Member metals Middle miles minerals minor natural norites occur outcrop Pakistan pegmatite Peshawar phyllites places plagioclase present probably quartz quartzites rare region result River road rocks samples schists seen sericite shale shear slates solubility solutions southern stream strike structure suggest sulphide Swat temperature thick thin transport types Univ Upper usually valley varieties various veins village volcanic waters western zone