Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
The colour of limestone ranges from light green, cream, dark grey to black. lt is
also brittle and gives foetid smell on breaking. They show sharp basal contact in
the thinly bedded sequence, whereas low relief erosional surfaces are present in
...
The colour of limestone ranges from light green, cream, dark grey to black. lt is
also brittle and gives foetid smell on breaking. They show sharp basal contact in
the thinly bedded sequence, whereas low relief erosional surfaces are present in
...
Page 151
The limestone band occurring above the quartzite is hard, grey with bands of
gritty calcareous quartzite. The limestone contains chunks and pebbles of vein
quartz and quartzite. There is apparently no discordance between the Ramban
and ...
The limestone band occurring above the quartzite is hard, grey with bands of
gritty calcareous quartzite. The limestone contains chunks and pebbles of vein
quartz and quartzite. There is apparently no discordance between the Ramban
and ...
Page 155
The beds about I80 meters thick comprise a basal conglomerate followed by 30
m thick siliceous shales, quartzite, carbonaceous shales and I27 m thick hard
grey quartzitic sandstone with ill preserved Lower Gondwana flora. In Kashmir ...
The beds about I80 meters thick comprise a basal conglomerate followed by 30
m thick siliceous shales, quartzite, carbonaceous shales and I27 m thick hard
grey quartzitic sandstone with ill preserved Lower Gondwana flora. In Kashmir ...
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Contents
Cnouasv KEWAL K SHARMA D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 21 |
G S MEHROTRA S SARKAR D P KANUNGO A geological appraisal of Landslide Hazards | 35 |
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Common terms and phrases
02:53 IST MAGNITUDE acanthomorphic acritarchs Agglomeratic Slate Amritpur axial plane Bafliaz Formation band basin biotite Budhal calcite chert classified clasts conglomerate defined deformation Dehra Dun deposits diamictite dolomite Doushantuo Formation Dum Gali Quartzite facies fault plane feldspar fi'om field figure fine first flank flows folds foliation fossils Garhwal Geol glacial gneiss granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation lndia lnfrakrol metamorphic Nappe ofthe Panjal thrust Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone schist sector sedimentary sediments sequence shale Sharma shear Shergol significance SiO2 slide slip slope soil stratigraphic structures Surv Suture Zone tectonic Tethyan Thakur thick Thinly bedded Uhl valley unconformably upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Zanskar