Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
... 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 section . 31 ° amur Algar Fault ...
... 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 section . 31 ° amur Algar Fault ...
Page 188
... fault plane was assumed . The slip vectors were oriented in accordance with the fault plane solution estimated for the earthquake . The amplitudes , and the orientations of these slip vectors over the fault plane ( rake ) were treated ...
... fault plane was assumed . The slip vectors were oriented in accordance with the fault plane solution estimated for the earthquake . The amplitudes , and the orientations of these slip vectors over the fault plane ( rake ) were treated ...
Page 189
... fault plane , in general , display low values of slip . In this region numerous aftershocks have occurred ( Fig . 2 ) . On the other hand , the regions which have shown large slip have not produced aftershocks . The areas of large slip ...
... fault plane , in general , display low values of slip . In this region numerous aftershocks have occurred ( Fig . 2 ) . On the other hand , the regions which have shown large slip have not produced aftershocks . The areas of large slip ...
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