Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 108
They trend in N - S , NNE - SSW and in ENE - WSW directions in the present area
. Subsequently the rocks were also folded , during which intergranular slip took
place in rocks of deeper zone and formed S2 ( S , = S2 ) . The presence of two ...
They trend in N - S , NNE - SSW and in ENE - WSW directions in the present area
. Subsequently the rocks were also folded , during which intergranular slip took
place in rocks of deeper zone and formed S2 ( S , = S2 ) . The presence of two ...
Page 121
The schistose quartzites of Dudatoli Group are marked by the presence of '
Almost Box ' and ' Multiple ' folds and absence of ' Sine wave ' and ' Cuspate '
folds , whereas the first two types are absent and the later two types are present
in the ...
The schistose quartzites of Dudatoli Group are marked by the presence of '
Almost Box ' and ' Multiple ' folds and absence of ' Sine wave ' and ' Cuspate '
folds , whereas the first two types are absent and the later two types are present
in the ...
Page 135
Constituent formations of ' Simla group ' and their correlative positions as per
different authors ( with minor modifications to bring uniformity and clarity ) Pilgrim
Present Srikantia Karunakaran & Medlicott and West Auden Authors and Sharma
...
Constituent formations of ' Simla group ' and their correlative positions as per
different authors ( with minor modifications to bring uniformity and clarity ) Pilgrim
Present Srikantia Karunakaran & Medlicott and West Auden Authors and Sharma
...
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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