Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
... 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 fault plane solution , with strike 317o , dip 14o , and slip ...
... 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 fault plane solution , with strike 317o , dip 14o , and slip ...
Page 175
... seismograms that are low pass filtered at 5 Hz may reasonably be modeled in a deterministic manner . One may obtain a corresponding slip function distribution on the fault by inverting this smoother component of observed ground motions ...
... seismograms that are low pass filtered at 5 Hz may reasonably be modeled in a deterministic manner . One may obtain a corresponding slip function distribution on the fault by inverting this smoother component of observed ground motions ...
Page 180
... seismogram . The waveforms on the left are for the parallel components , and on the right for the parallel components ... seismograms of the earthquakes the predominant phases are the P and S body waves . The computational effort may be ...
... seismogram . The waveforms on the left are for the parallel components , and on the right for the parallel components ... seismograms of the earthquakes the predominant phases are the P and S body waves . The computational effort may be ...
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