Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 185
Slip vector Distribution 0 Along Fault Strike ( km ) Fig . 9 ( c ) . The slip vector
distribution for rise time of 0.3s . Total Slip Amplitude Distribution and Rupture
Time Contour o 5. o 5 ( km ) Dip 10 Foult Along 15 20 -10 10 with error
covariance ...
Slip vector Distribution 0 Along Fault Strike ( km ) Fig . 9 ( c ) . The slip vector
distribution for rise time of 0.3s . Total Slip Amplitude Distribution and Rupture
Time Contour o 5. o 5 ( km ) Dip 10 Foult Along 15 20 -10 10 with error
covariance ...
Page 188
One of the approaches to study the fault heterogeneity is to infer slip distributions
from earthquake seismograms . The near source ... The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
...
One of the approaches to study the fault heterogeneity is to infer slip distributions
from earthquake seismograms . The near source ... The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
...
Page 189
The corresponding slip distribution is shown in figure 9b . The pattern of slip
distribution is similar as in the previous cases , though the slip amplitudes and
areas of larger slip have been reduced further as compared to the previous cases
.
The corresponding slip distribution is shown in figure 9b . The pattern of slip
distribution is similar as in the previous cases , though the slip amplitudes and
areas of larger slip have been reduced further as compared to the previous cases
.
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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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Common terms and phrases
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