Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 51
If one takes 1500 km for the east - west dimension and 800 km for the average
north - south dimension of this region ( area = 1.2 x 106 km2 ) , and 15 km for the
thickness of the seismogenic layer , the calculated rate of east - west extension ...
If one takes 1500 km for the east - west dimension and 800 km for the average
north - south dimension of this region ( area = 1.2 x 106 km2 ) , and 15 km for the
thickness of the seismogenic layer , the calculated rate of east - west extension ...
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 -
east , they ...
( 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 -
east , they ...
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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 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