Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 43
East - west crustal extension characterizes the high plateau ; normal faulting
along roughly north - south trending grabens allows the south - eastern and
south - western extremities of the plateau to move apart at about 19 + 9 mm / a ...
East - west crustal extension characterizes the high plateau ; normal faulting
along roughly north - south trending grabens allows the south - eastern and
south - western extremities of the plateau to move apart at about 19 + 9 mm / a ...
Page 49
East - west crustal extension characterizes the high plateau ; normal faulting
along roughly north - south trending grabens allows the south - eastern and
south - western extremities of the plateau to move apart at about 19 + 9 mm / a ...
East - west crustal extension characterizes the high plateau ; normal faulting
along roughly north - south trending grabens allows the south - eastern and
south - western extremities of the plateau to move apart at about 19 + 9 mm / a ...
Page 59
Using 330 m and 18 ka yields 18 mm / a . This rate suggests that there was rapid
erosion at 11 to 14 ka , when the large number of features now offset 200-250m
formed . Recall that , at 10-12 ka , a relatively wet climate prevailed in the ...
Using 330 m and 18 ka yields 18 mm / a . This rate suggests that there was rapid
erosion at 11 to 14 ka , when the large number of features now offset 200-250m
formed . Recall that , at 10-12 ka , a relatively wet climate prevailed in the ...
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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