Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 139
Photograph showing preferred orientation of pebbles on the cleavage plane
developed in the conglomerate at Shergol, Ladakh, J & K. where u oct is a
measure of the magnitude of distortional component. The value of 7 can be
expressed as ...
Photograph showing preferred orientation of pebbles on the cleavage plane
developed in the conglomerate at Shergol, Ladakh, J & K. where u oct is a
measure of the magnitude of distortional component. The value of 7 can be
expressed as ...
Page 143
In the Hsu diagam, Es and u - values of all the pebbles fiom different locations
indicate no definite pattern. The magnitude of strain (Es) of the pebbles of similar
composition varies over a wide range of values in different locations (Table 3).
In the Hsu diagam, Es and u - values of all the pebbles fiom different locations
indicate no definite pattern. The magnitude of strain (Es) of the pebbles of similar
composition varies over a wide range of values in different locations (Table 3).
Page 144
Strain analysis of pebbles of conglomerate shows that the shape of the pebbles
varies from constrictional type to the flattening type. The pebbles which are
comparatively less competent show more flattening type of strain whereas the
pebbles ...
Strain analysis of pebbles of conglomerate shows that the shape of the pebbles
varies from constrictional type to the flattening type. The pebbles which are
comparatively less competent show more flattening type of strain whereas the
pebbles ...
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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