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 Lj - lineation from the ...
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 Lj - lineation from the ...
Page 44
Most of these studies, and particularly the earlier ones, began with two implicit
assumptions: rotations about vertical axes do not play a major part in the
deformation of Tibet, and slip on faults reflects an effectively rigid-body
displacement of ...
Most of these studies, and particularly the earlier ones, began with two implicit
assumptions: rotations about vertical axes do not play a major part in the
deformation of Tibet, and slip on faults reflects an effectively rigid-body
displacement 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 suffered
at ...
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 suffered
at ...
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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