Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 22
The Giumal Formation is succeeded disconformably by the Goma Formation
which comprises black shale with lenses of limestone in the lower and middle
parts, and marl and shale with subordinate limestone in the upper one. The
Goma ...
The Giumal Formation is succeeded disconformably by the Goma Formation
which comprises black shale with lenses of limestone in the lower and middle
parts, and marl and shale with subordinate limestone in the upper one. The
Goma ...
Page 69
Trace fossils, burrows and trails are common in upper succession of marl facies.
They also show at places gradational contact with limestone. The sandstone with
shale and limestone is present at various stratigraphic levels in the upper part ...
Trace fossils, burrows and trails are common in upper succession of marl facies.
They also show at places gradational contact with limestone. The sandstone with
shale and limestone is present at various stratigraphic levels in the upper part ...
Page 120
Morainic deposit covered by taluses south of Kukurgundha eroded by the Uhl
river on upper and lateral side. the upper part of the valley, about one km north of
Palachak, morainic deposits consist of weathered erratic boulders of granite, ...
Morainic deposit covered by taluses south of Kukurgundha eroded by the Uhl
river on upper and lateral side. the upper part of the valley, about one km north of
Palachak, morainic deposits consist of weathered erratic boulders of granite, ...
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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