Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 175
Analytical Framework for Inversion The elastodynamic radiation from an
earthquake source at frequencies lower than about 5 Hz are assumed to be
given by relatively coherent component of slip over the fault plane and are
considered to ...
Analytical Framework for Inversion The elastodynamic radiation from an
earthquake source at frequencies lower than about 5 Hz are assumed to be
given by relatively coherent component of slip over the fault plane and are
considered to ...
Page 187
We model the rupture by a fault plane with the following parameters. Strike: 317°;
Dip ; 14° to the NE; Slip: 115° The dimensions of the planer fault chosen for
modeling are 30x20 km, which is based on the extent of the afiershock zone, and
the ...
We model the rupture by a fault plane with the following parameters. Strike: 317°;
Dip ; 14° to the NE; Slip: 115° The dimensions of the planer fault chosen for
modeling are 30x20 km, which is based on the extent of the afiershock zone, and
the ...
Page 188
To begin the inversion for earthquake 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.
To begin the inversion for earthquake 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.
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Contents
Cnouasv KEWAL K SHARMA D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 21 |
G S MEHROTRA S SARKAR D P KANUNGO A geological appraisal of Landslide Hazards | 35 |
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02:53 IST MAGNITUDE acanthomorphic acritarchs Agglomeratic Slate Amritpur axial plane Bafliaz Formation band basin biotite Budhal calcite chert classified clasts conglomerate defined deformation Dehra Dun deposits diamictite dolomite Doushantuo Formation Dum Gali Quartzite facies fault plane feldspar fi'om field figure fine first flank flows folds foliation fossils Garhwal Geol glacial gneiss granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation lndia lnfrakrol metamorphic Nappe ofthe Panjal thrust Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone schist sector sedimentary sediments sequence shale Sharma shear Shergol significance SiO2 slide slip slope soil stratigraphic structures Surv Suture Zone tectonic Tethyan Thakur thick Thinly bedded Uhl valley unconformably upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Zanskar