Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 74
On the left , a simple arrangement of rigid blocks separated by planer faults is used to compare simple left - lateral shear without rotation ( top ) with rotations of blocks in a zone of rightlateral regional shear ( bottom ) .
On the left , a simple arrangement of rigid blocks separated by planer faults is used to compare simple left - lateral shear without rotation ( top ) with rotations of blocks in a zone of rightlateral regional shear ( bottom ) .
Page 92
blocks of igneous , sedimentary and metamorphic parentage chaotically mixed together in a complex manner . The south or SE dipping blocks are imbricately arranged within the disrupted terrigenous turbiditic matrix , which are ...
blocks of igneous , sedimentary and metamorphic parentage chaotically mixed together in a complex manner . The south or SE dipping blocks are imbricately arranged within the disrupted terrigenous turbiditic matrix , which are ...
Page 187
These together with blocks that may have come from a continental shelf and slope ( Sinha & Upadhyay , 1990 , 1993 ) ... The blocks and slices in the ophiolitic melange corresponds to the deposits of highly contrasting environments ranging ...
These together with blocks that may have come from a continental shelf and slope ( Sinha & Upadhyay , 1990 , 1993 ) ... The blocks and slices in the ophiolitic melange corresponds to the deposits of highly contrasting environments ranging ...
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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 analysis 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