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 right , the same ...
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 right , the same ...
Page 92
blocks of igneous , sedimentary and metamorphic parentage chaotically mixed
together in a complex manner . The south or SE SE dipping blocks are
imbricately arranged within the disrupted terrigenous turbiditic matrix , which are
interpreted ...
blocks of igneous , sedimentary and metamorphic parentage chaotically mixed
together in a complex manner . The south or SE SE dipping blocks are
imbricately arranged within the disrupted terrigenous turbiditic matrix , which are
interpreted ...
Page 185
Another conglomerate block exposed at Shergol village exhibits a significant
contrast between submarine and subaerial ... from all the lithologies along the
Indus Suture zone with blocks measuring upto 250 cm lying in silty to clayey
matrix .
Another conglomerate block exposed at Shergol village exhibits a significant
contrast between submarine and subaerial ... from all the lithologies along the
Indus Suture zone with blocks measuring upto 250 cm lying in silty to clayey
matrix .
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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