Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 10
It is also observed that the abundances of Ga , Nb and Pb in these rocks are within the range of average crustal rocks ( Taylor , 1964 ) . This character and the metasedimentary nature of these rocks indicate that they are derived from ...
It is also observed that the abundances of Ga , Nb and Pb in these rocks are within the range of average crustal rocks ( Taylor , 1964 ) . This character and the metasedimentary nature of these rocks indicate that they are derived from ...
Page 141
both Upper Murree and Lower Siwalik rocks in this structural unit are represented by very coarse facies - often pebbly and gritty at places . In the area under reference , the authors have not observed Lower Siwalik rocks in Mudun ...
both Upper Murree and Lower Siwalik rocks in this structural unit are represented by very coarse facies - often pebbly and gritty at places . In the area under reference , the authors have not observed Lower Siwalik rocks in Mudun ...
Page 197
Thrusted over these Upper Siwalik conglomerates along the MT , lie the Lower Miocene rocks of Murree Formation . The Murree rocks , which have been correlated with Dharmashala , KasauliDagshai and Tipam - Surma ( Wadia , 1957 ; Mathur ...
Thrusted over these Upper Siwalik conglomerates along the MT , lie the Lower Miocene rocks of Murree Formation . The Murree rocks , which have been correlated with Dharmashala , KasauliDagshai and Tipam - Surma ( Wadia , 1957 ; Mathur ...
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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 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