Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 66
Estimating the average displacement on the 300 km zone is difficult , and assigning it to one ( or two ) earthquakes is risky . First , note that the events of 1963 and 1971 probably could not have contributed much to this long rupture ...
Estimating the average displacement on the 300 km zone is difficult , and assigning it to one ( or two ) earthquakes is risky . First , note that the events of 1963 and 1971 probably could not have contributed much to this long rupture ...
Page 70
( 1991 ) found offsets of 3 m that they could Perhaps a safe way to state the average Holocene slip confidently associate with the 1923 earthquake and rate is as 18 + 7 mm / a ( Molnar et al . 1976 ) , a range some 36 km farther south ...
( 1991 ) found offsets of 3 m that they could Perhaps a safe way to state the average Holocene slip confidently associate with the 1923 earthquake and rate is as 18 + 7 mm / a ( Molnar et al . 1976 ) , a range some 36 km farther south ...
Page 71
A value of 7.4 10'8Nm suggests an average displacement of 0.27 ( + 0.1 ) m for an average width of 20 km . Seismic slip rate al . 1991 ) . An average displacement of 1.5 + 0.5 m corresponds to a scalar seismic moment of 2.7 ( + 1.35 ) X ...
A value of 7.4 10'8Nm suggests an average displacement of 0.27 ( + 0.1 ) m for an average width of 20 km . Seismic slip rate al . 1991 ) . An average displacement of 1.5 + 0.5 m corresponds to a scalar seismic moment of 2.7 ( + 1.35 ) X ...
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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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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