Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
This facies is generally thinly bedded and bed thickness increases towards top.
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 ...
This facies is generally thinly bedded and bed thickness increases towards top.
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 ...
Page 121
/Oflern boulders rum llopq Ollllutllon lobe; g Wash flops Fig. 6. Typical cross-
section of the Uhl Valley showing glacial and periglacial material. thick soil
horizon has distinct black and brown soil layers buried under 40-60 cm thick
recent soil.
/Oflern boulders rum llopq Ollllutllon lobe; g Wash flops Fig. 6. Typical cross-
section of the Uhl Valley showing glacial and periglacial material. thick soil
horizon has distinct black and brown soil layers buried under 40-60 cm thick
recent soil.
Page 155
Panjal Volcanic Formation: The Agglomeratic Slate along with Gondwana plant
bearing beds towards its top are overlain by a thick pile of lava flows designated
as Panjal Volcanics forming the summit zone of Pir Panjal range. lt forms steep ...
Panjal Volcanic Formation: The Agglomeratic Slate along with Gondwana plant
bearing beds towards its top are overlain by a thick pile of lava flows designated
as Panjal Volcanics forming the summit zone of Pir Panjal range. lt forms steep ...
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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