Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 133
... pebbles of limestone , slate and serpentine are triaxial flattening type ellipsoids , while pebbles of argillaceous sandstone , basalt and gabbro show large variation of shape . There is a strong preferred orientation of long axes ...
... pebbles of limestone , slate and serpentine are triaxial flattening type ellipsoids , while pebbles of argillaceous sandstone , basalt and gabbro show large variation of shape . There is a strong preferred orientation of long axes ...
Page 139
... Pebbles are poorly sorted and constitute about 75 % of the whole rock on an average . The pebbles are more or less ellipsoidal in shape with longest axes ranging from 0.5 to 15 cm . Thakur and Misra ( 1984 ) have reported pebbles of ...
... Pebbles are poorly sorted and constitute about 75 % of the whole rock on an average . The pebbles are more or less ellipsoidal in shape with longest axes ranging from 0.5 to 15 cm . Thakur and Misra ( 1984 ) have reported pebbles of ...
Page 144
... 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 which are ...
... 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 which are ...
Contents
CHOUBEY Kewal K Sharma D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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02:53 IST MAGNITUDE Accel cm/sē Agglomeratic Slate Amritpur axial plane Bafliaz Formation basin biotite Budhal Burtsa Formation calcite chert clasts conglomerate Cretaceous deformation Dehra Dun deposits dolomite Dum Gali Quartzite facies fault plane feldspar folds foliation fossils Garhwal Geol gneiss grained granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology India Infrakrol Institute of Himalayan inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation Maastrichtian Mandi metamorphic Nappe Nilkanth Panjal thrust Panjal Volcanic Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone Sarkanth schist sector sedimentary sediments sequence shale Sharma shear Shergol Singh SiO2 slide slip slope soil strain Stratigraphy structures Surv Suture Zone Syncline tectonic Tethyan Thakur thick Thinly bedded Uhl valley Unconformity upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Ypresian Zanskar