Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
From inside the book
Results 1-3 of 34
Page 34
The earliest mention of the Gandghar Range was made by Middlemiss ( 1896 )
while describing the marmorised and brecciated limestone associated with the
Hazara Slate Series , showing peculiar stromato - poroidal structure .
The earliest mention of the Gandghar Range was made by Middlemiss ( 1896 )
while describing the marmorised and brecciated limestone associated with the
Hazara Slate Series , showing peculiar stromato - poroidal structure .
Page 63
usually closely associated with hornblende . Micas are rare in these granites , but
when present , they are generally in very small amounts . They are commonly
biotite or muscovite , and occur as small strained laths , tappering at one end .
usually closely associated with hornblende . Micas are rare in these granites , but
when present , they are generally in very small amounts . They are commonly
biotite or muscovite , and occur as small strained laths , tappering at one end .
Page 65
Another body costitutes the Tora Tiga ( Black hill ) complex , wbere it is
associated with pyroxenites and peridotites . The third largest body is in the south
- central part , between Tabai and Chinghəz banda , north of Babukara Khawar .
Another body costitutes the Tora Tiga ( Black hill ) complex , wbere it is
associated with pyroxenites and peridotites . The third largest body is in the south
- central part , between Tabai and Chinghəz banda , north of Babukara Khawar .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Preliminary geology and petrography of Swat Kohistan EARTH | 1 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
Lithological classification and environment of deposition of | 43 |
6 other sections not shown
Other editions - View all
Common terms and phrases
abundant amounts amphibolites appears associated bands base beds biotite body brines Bull carbonates changes chlorite colour common complexes composition concentration contain correlated crystals dark deposits developed diorites dykes east eastern epidote exposed extend feet feldspar fluids folded Formation fractures Gandghar Range Geol geology grades grains granites green grey Group hornblende hydrothermal inclusions increases Indus intrusions iron Kalam latter layers light limestone locally located Lower marble material Member metals Middle miles minerals nature norites occur origin outcrop Pakistan pegmatite Peshawar phyllites places plagioclase present probably quartz quartzite rare region result River road rocks samples schists seen sericite shale sheared shown Slates solubility solutions stream strike structure suggested sulphide sulphur Swat temperature thick thin transport types Univ Upper usually valley varieties various veins village volcanic waters western zone