Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 163
A low angle thrust fault plane solution , with strike 317o , dip 14 ° , and slip 115o
was used in the inversion model . The slip distribution obtained indicates that the
slip was highest in two localities , one around the hypocenter , and the other ...
A low angle thrust fault plane solution , with strike 317o , dip 14 ° , and slip 115o
was used in the inversion model . The slip distribution obtained indicates that the
slip was highest in two localities , one around the hypocenter , and the other ...
Page 188
This will be of .considerable utility in earthquake hazard parameterization . over
the fault plane in the form of variable density plots . The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
1 ...
This will be of .considerable utility in earthquake hazard parameterization . over
the fault plane in the form of variable density plots . The ( c ) parts of the figures
show the slip vector distribution over the fault plane . For the choice of rise time of
1 ...
Page 189
This is seen in the form of north - east trending zones of higher strength
interpressed with zones of lower strength in the region of the fault plane .
Although the estimated depth of focus of the earthquake is 12 km , which is
higher than the ...
This is seen in the form of north - east trending zones of higher strength
interpressed with zones of lower strength in the region of the fault plane .
Although the estimated depth of focus of the earthquake is 12 km , which is
higher than the ...
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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