Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Printed in India Fault bifurcation : Evidence for reversal of fault displacement A. K.
DUBEY Wadia Institute of Himalayan Geology , Dehra Dun - 248001 , India
Abstract : A mesoscopic fault from the low grade metasedimentary sequence of
the ...
Printed in India Fault bifurcation : Evidence for reversal of fault displacement A. K.
DUBEY Wadia Institute of Himalayan Geology , Dehra Dun - 248001 , India
Abstract : A mesoscopic fault from the low grade metasedimentary sequence of
the ...
Page 4
The maximum displacement took place in the central part of the fracture and the
fault terminated by curvature towards the receding side . A number of other
extensional fractures also initiated in the model . Fig . 7B . The same multilayer
model ...
The maximum displacement took place in the central part of the fracture and the
fault terminated by curvature towards the receding side . A number of other
extensional fractures also initiated in the model . Fig . 7B . The same multilayer
model ...
Page 194
The overall sense of displacement is sinistral and shear plane strikes 330 ° 10
350 ° i.e. , from NNW to SSE with an average dip of 30 ° due north . The Tethyan
Thrust has been folded by D3 phase of deformation along with Rohtang antiform
...
The overall sense of displacement is sinistral and shear plane strikes 330 ° 10
350 ° i.e. , from NNW to SSE with an average dip of 30 ° due north . The Tethyan
Thrust has been folded by D3 phase of deformation along with Rohtang antiform
...
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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