Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 56
3 ) , along which central and northern Tibet are extruded eastward . This system
of right - lateral faults seems to lie near the boundary between southernmost
Tibet , where normal faulting is dominant , and central and northern Tibet , where
...
3 ) , along which central and northern Tibet are extruded eastward . This system
of right - lateral faults seems to lie near the boundary between southernmost
Tibet , where normal faulting is dominant , and central and northern Tibet , where
...
Page 145
( 2 ) Size sorting ( sd ) with respect to " a " axis , from poor sorting ( high values )
at the central zone of the map area decreases sharply to the NE and SW ,
commensurate with the variation in " a " axis measurements . The 3rd order fit for
sd , " b ...
( 2 ) Size sorting ( sd ) with respect to " a " axis , from poor sorting ( high values )
at the central zone of the map area decreases sharply to the NE and SW ,
commensurate with the variation in " a " axis measurements . The 3rd order fit for
sd , " b ...
Page 146
There is a northwest to southeast low in the central part of the map with a closure
of high values at the northwest and low values at the southeast extremities of the
map . ( 6 ) The limestone sixth order surface shows a central low trend ( NW ...
There is a northwest to southeast low in the central part of the map with a closure
of high values at the northwest and low values at the southeast extremities of the
map . ( 6 ) The limestone sixth order surface shows a central low trend ( NW ...
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Contents
Fold shape analysis in the vicinity of North Almora Thrust in District | 121 |
Simla group problem in HimalayaA critical review | 131 |
Geology of Kishanpur NagrotaBasantgarhGujru Nagrota Sector of Inner | 137 |
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Common terms and phrases
active associated average axis beds belt blocks central Chevron Folds compressive stresses crustal deformation developed direction displacement earthquake east east-west eastern estimated et al evidence exposed extension fault field folds Formation formed Garhwal Geol Geology grains granite Group Himalaya Himalayan Geology India indicate Jammu Jour landslide lateral left-lateral limestone lineation Lower major margin measurements melange metamorphism Mineral mm/a Molnar movement Murree normal faulting northern observed occurred oceanic offset ophiolitic orientation phase plane plateau Pradesh present pressure quartz quartzite range References region reported represent result rocks roughly samples sandstones seismic sequence Shan shape shear shortening Simla Sine Waves Siwalik Slates slip solutions southern specimens strain strike-slip faulting structures suggest surface Table Tapponnier tectonic thrust thrust faulting Tibet trending types units Upper valley volcanics western zone