Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
... higher in the down dip region of the fault plane , with the slip diminishing in the up dip direction . The aftershocks population is higher in the up dip section of the fault plane correlating with the main shock slip deficiency in that ...
... higher in the down dip region of the fault plane , with the slip diminishing in the up dip direction . The aftershocks population is higher in the up dip section of the fault plane correlating with the main shock slip deficiency in that ...
Page 189
... higher strength interpressed with zones of lower strength in the region of the fault plane . Although the estimated depth of focus of the earthquake is 12 km , which is higher than the projected depth of detachment estimated at 18-22 km ...
... higher strength interpressed with zones of lower strength in the region of the fault plane . Although the estimated depth of focus of the earthquake is 12 km , which is higher than the projected depth of detachment estimated at 18-22 km ...
Page 197
... higher magnification . 6. Unclassified acanthomorphic acritarch WIMF / A 1029 , sample no . MT / CH / GUN / 4-3 . 6a . Detail of same specimen at higher magnification . 7. Siphonophycus inomatum WIMF / A 1030 , sample no . MT / NG / 1-1 ...
... higher magnification . 6. Unclassified acanthomorphic acritarch WIMF / A 1029 , sample no . MT / CH / GUN / 4-3 . 6a . Detail of same specimen at higher magnification . 7. Siphonophycus inomatum WIMF / A 1030 , sample no . MT / NG / 1-1 ...
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/s² 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