Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 72
Hence , this lower inferred rate does not necessarily indicate an important variation in the rate of slip along the fault zone . The total offset on the Xianshuihe fault has not been measured definitively .
Hence , this lower inferred rate does not necessarily indicate an important variation in the rate of slip along the fault zone . The total offset on the Xianshuihe fault has not been measured definitively .
Page 163
Results available so far indicate predominance of thrust faulting along the entire belt . A few earthquakes indicated normal faulting in a manner similar to the tension in the down going slab . The Burma - India border region was ...
Results available so far indicate predominance of thrust faulting along the entire belt . A few earthquakes indicated normal faulting in a manner similar to the tension in the down going slab . The Burma - India border region was ...
Page 205
1 ) the Salkhala Formation ( PT sheet ) directly overlies the Murrees , indicating that the PT as the roof thrust comes to join the MBT as ... The MBT and the MT showing pulverisation near the contact zone indicate brittle deformation .
1 ) the Salkhala Formation ( PT sheet ) directly overlies the Murrees , indicating that the PT as the roof thrust comes to join the MBT as ... The MBT and the MT showing pulverisation near the contact zone indicate brittle deformation .
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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