Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 140
The sandstone is fine to medium grained in the basal part and gradually
becomes coarser in the upper part. It breaks into large blocks along well
developed joint planes. The sandstones exhibit well developed current bedding,
ripple marks, ...
The sandstone is fine to medium grained in the basal part and gradually
becomes coarser in the upper part. It breaks into large blocks along well
developed joint planes. The sandstones exhibit well developed current bedding,
ripple marks, ...
Page 138
( 4 - Conglomerate beds ) Upper Murree ( Upper Eocene to Lower Miocene ; 5 .
ower Siwalik ; 6. Middle Siwalik ; 7. Upper Siwalik ( Mid Miocene to Lower
Pleistocene ) ; 8. Alluvium and Terrace deposit ( Sub - Recent to Recent ) .
Journal of ...
( 4 - Conglomerate beds ) Upper Murree ( Upper Eocene to Lower Miocene ; 5 .
ower Siwalik ; 6. Middle Siwalik ; 7. Upper Siwalik ( Mid Miocene to Lower
Pleistocene ) ; 8. Alluvium and Terrace deposit ( Sub - Recent to Recent ) .
Journal of ...
Page 140
The sandstone is fine to medium grained in the basal part and gradually
becomes coarser in the upper part . It breaks into large blocks along well
developed joint planes . The sandstones exhibit well developed current bedding ,
ripple marks ...
The sandstone is fine to medium grained in the basal part and gradually
becomes coarser in the upper part . It breaks into large blocks along well
developed joint planes . The sandstones exhibit well developed current bedding ,
ripple marks ...
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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