Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 18
The pre - deformation pattern of the vesicles was random as evidenced in the Rf / $ plot . The vectorial mean ( Cheeny , 1985 ) of the largest axes of the three deformed vesicular markers along with the other kinds of L , -lineation ...
The pre - deformation pattern of the vesicles was random as evidenced in the Rf / $ plot . The vectorial mean ( Cheeny , 1985 ) of the largest axes of the three deformed vesicular markers along with the other kinds of L , -lineation ...
Page 44
Further quantification of the rates of slip on these faults strengthened convictions that slip on them plays an important role in the deformation of eastern Tibet and that material is displaced rapidly eastward out of ...
Further quantification of the rates of slip on these faults strengthened convictions that slip on them plays an important role in the deformation of eastern Tibet and that material is displaced rapidly eastward out of ...
Page 203
The microstructures indicate intense non - coaxial deformation which has caused the PT sheet to overlie the Shali rocks along a thrusted contact , the PT . It is evident from the microstructural and mesoscopic evidences that the area ...
The microstructures indicate intense non - coaxial deformation which has caused the PT sheet to overlie the Shali rocks along a thrusted contact , the PT . It is evident from the microstructural and mesoscopic evidences that the area ...
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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 Jour landslide lateral left-lateral limestone lineation Lower major margin measurements melange metamorphism Mineral mm/a Molnar movement Murree ND ND ND normal faulting northern observed occurred oceanic offset ophiolitic orientation phase plane plateau present pressure quartz quartzite range References region reported represent result rocks roughly samples sandstones seismic 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