Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
... estimated by inverting the near - source strong ground motion seismograms . Forward modelling has been done using the isochrone method , and for linear inversion recursive stochastic inverse algorithm has been used . A low angle thrust ...
... estimated by inverting the near - source strong ground motion seismograms . Forward modelling has been done using the isochrone method , and for linear inversion recursive stochastic inverse algorithm has been used . A low angle thrust ...
Page 188
... estimated for the earthquake . The amplitudes , and the orientations of these slip vectors over the fault plane ( rake ) were treated as the parameters for estimation in the inversion procedure . Thus , the distribution of source slip ...
... estimated for the earthquake . The amplitudes , and the orientations of these slip vectors over the fault plane ( rake ) were treated as the parameters for estimation in the inversion procedure . Thus , the distribution of source slip ...
Page 189
... estimated is 300 cm . The moment obtained in this case is also smaller than that obtained from teleseismic data ... estimated depth of focus of the earthquake is 12 km , which is higher than the projected depth of detachment estimated at ...
... estimated is 300 cm . The moment obtained in this case is also smaller than that obtained from teleseismic data ... estimated depth of focus of the earthquake is 12 km , which is higher than the projected depth of detachment estimated at ...
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