Kn. Khattri, A SEISMIC HAZARD AND RISK SCENARIO FOR HIMALAYA AND GANGA PLAINS DUE TO A FUTURE GREAT EARTHQUAKE, National Academy Science Letters, 21(5-6), 1998, pp. 193-220
Strong ground motion time histories are synthesized using the composit
e source model at a few sites for a prototype gap filling Mw 8.5 great
earthquake in the western side of the central seismic gap in Himalaya
which extends from the Bhagirathi valley in the west to the Kali vall
ey in the east. The peak ground accelerations attain values around 1 g
in the regions overlying the fault plane. In the Ganga plains the val
ues vary from 0.32 g to 0.7 g depending on the distance from the fault
plane. The damage potential of such an earthquake is extreme. The pos
sibilities of its compounding due to failure civil works like high dam
s exist. The loss of human lives could be over several hundred thousan
d and economic loss of hundreds of billion Rupees. A further scenario
was developed for an extentional type of earthquake (M-w 6) in the Gan
ga foredeep at a short epicentral distance. This showed that peak grou
nd acceleration of about 0.32 g can be produced exposing the effected
regions to considerable hazard.