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 the
partial ...
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 the
partial ...
Page 58
Photograph looking north - northeast at a thrust fault scarp , shown by the white
and black arrows , above which a perched alluvial fan is now eroding . The range
behind is the Akato Tagh , near 38.2 ° N , 89.7 ° E ( See Molnar et al . , 1987b ) .
Photograph looking north - northeast at a thrust fault scarp , shown by the white
and black arrows , above which a perched alluvial fan is now eroding . The range
behind is the Akato Tagh , near 38.2 ° N , 89.7 ° E ( See Molnar et al . , 1987b ) .
Page 158
The halite melting between 210 ° to 250 ° C correspond to the salinity range of 32
10 34.5 wt . percent NaCl equiv . The homogenization into liquid phase between
300 to 410 ° C ( Fig . 7b ) combined with salinity data would provide density ...
The halite melting between 210 ° to 250 ° C correspond to the salinity range of 32
10 34.5 wt . percent NaCl equiv . The homogenization into liquid phase between
300 to 410 ° C ( Fig . 7b ) combined with salinity data would provide density ...
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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