Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
... slip 115 ° was used in the inversion model . The slip distribution obtained indicates that the slip was highest in two localities , one around the hypocenter , and the other , the larger , further westward . The latter was the strongest ...
... slip 115 ° was used in the inversion model . The slip distribution obtained indicates that the slip was highest in two localities , one around the hypocenter , and the other , the larger , further westward . The latter was the strongest ...
Page 188
... slip in the present analysis , a uniform distribution of the initial slip over the fault plane was assumed . The slip vectors were oriented in accordance with the fault plane solution estimated for the earthquake . The amplitudes , and ...
... slip in the present analysis , a uniform distribution of the initial slip over the fault plane was assumed . The slip vectors were oriented in accordance with the fault plane solution estimated for the earthquake . The amplitudes , and ...
Page 189
patches with higher slip displaying a combination of comparable dip and strike slips . The synthetic seismograms for ... slip distribution is shown in figure 9b . The pattern of slip distribution is similar as in the previous cases ...
patches with higher slip displaying a combination of comparable dip and strike slips . The synthetic seismograms for ... slip distribution is shown in figure 9b . The pattern of slip distribution is similar as in the previous cases ...
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