Geological Bulletin, Volume 11University of Peshawar, 1979 - Geology |
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Page 12
... bodies mentioned in Thak nala ( Shams , 1975 ) in Chilas area and near Babu
Sar in the upper reaches of Kaghan in Hazara . Besides , many small bodies of
ultramafic rocks have been noticed strewing the metasediments and
amphibolites ...
... bodies mentioned in Thak nala ( Shams , 1975 ) in Chilas area and near Babu
Sar in the upper reaches of Kaghan in Hazara . Besides , many small bodies of
ultramafic rocks have been noticed strewing the metasediments and
amphibolites ...
Page 46
The talc appears to replace serpentine in some cases ; that steatisation follows
serpenlinisation has been noticed in other areas ( Jahns , 1967 , p . 155 ) . The
sequence of tremolite - serpentine formation is not clear . In some rocks the ...
The talc appears to replace serpentine in some cases ; that steatisation follows
serpenlinisation has been noticed in other areas ( Jahns , 1967 , p . 155 ) . The
sequence of tremolite - serpentine formation is not clear . In some rocks the ...
Page 174
At other places , like Benton tunnel - Malakand , granitic intrusions have been
noticed in the meta - hornblendites . It is therefore believed that the ultrabasic
activity prevailed over a considerable span of time with the last phases close to or
...
At other places , like Benton tunnel - Malakand , granitic intrusions have been
noticed in the meta - hornblendites . It is therefore believed that the ultrabasic
activity prevailed over a considerable span of time with the last phases close to or
...
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Common terms and phrases
abundant altered amphibole amphibolites anorthosite appears associated bands basic bedded belt biotite bodies Bull Chitral clinopyroxene common complex composition considered contain dark developed diorites east epidote exposed extend fault feldspar foliation Formation garnet Geol Geology Gilgit gneisses gneissose grains granitic granulites green grey Group Hazara Himalaya hornblende igneous inclusions Indus intrusions Jijal Kalam Khan Kohistan layers less light limestone locally located lower major margins mass material medium metamorphic Mian Middle minerals minor Nanga Parbat norites northern occur opaque origin Pakistan pegmatites Peshawar places plagioclase plate present probably pyroxene pyroxene granulites pyroxenites quartz quartzites range rare region reported result rocks schists sequence sericite slates southern stream structure studies suggest Swat Tahirkheli tectonic thick thin thrust traces trend twinning ultramafic Univ upper usually valley veins volcanic western zone ܘ ܘ ܘ