Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
Inversion of Strong Motion Waveforms for Source Slip function of 1991 Uttarkashi
Earthquake , Himalaya K.N. KHATTRI ' , YUEHUA ZENG ?, J.G. ANDERSON ? &
J. BRUNE2 Wadia Institute of Himalayan Geology , Dehra Dun , U.P. 248 001 ...
Inversion of Strong Motion Waveforms for Source Slip function of 1991 Uttarkashi
Earthquake , Himalaya K.N. KHATTRI ' , YUEHUA ZENG ?, J.G. ANDERSON ? &
J. BRUNE2 Wadia Institute of Himalayan Geology , Dehra Dun , U.P. 248 001 ...
Page 185
The matrix inversion can be replaced by an iterative scheme due Zeng ( 1991 ) .
Under the assumption that model and noise vectors obey joint Gaussian
distribution , the following set of recursive equations are obtained . în 1 + 1 = m +
H + 1 ...
The matrix inversion can be replaced by an iterative scheme due Zeng ( 1991 ) .
Under the assumption that model and noise vectors obey joint Gaussian
distribution , the following set of recursive equations are obtained . în 1 + 1 = m +
H + 1 ...
Page 188
Inversion parameters obtained for three choices of rise time . Rise time Moment
Rake ... The waveforms , the rupture time contour map , and the total slip
amplitude distribution for the above three inversions are shown in figures 7-9 . In
the ( a ) ...
Inversion parameters obtained for three choices of rise time . Rise time Moment
Rake ... The waveforms , the rupture time contour map , and the total slip
amplitude distribution for the above three inversions are shown in figures 7-9 . In
the ( a ) ...
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Contents
Petrogenesis of the Granitoid Rocks Chor Region Himachal Himalaya | 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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Agglomeratic Slate analysis associated band base basin bedded belt chert components composition comprising conglomerate contain covered deformation Dehra deposits developed direction distribution district earthquake et al exposed facies fault fault plane feldspar field folds foliation followed Formation fossils Garhwal Geol gneiss grained granites granitoids grey Group higher Himalaya Himalayan Geology India indicates inversion Jour Kashmir Ladakh Lamayuru Late Lesser limestone lineation locality locations lower major Member metamorphic minerals observed occur Panjal pebbles phase phyllites plagioclase plane Pleistocene porphyries present quartz quartzite range region reported represented river road rocks samples sandstone schist sector sedimentary sediments sequence shale Sharma shown Slate slide slip slope soil strain stratigraphy strike structures suggest Surv Table tectonic thick thrust trace unit upper valley VALUES Volcanics Wadia weathered Zanskar zone