Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 17
Page 37
... flow Burdang slide 30 33.5 Rock - cum- debris slide Rangpo slide 70 40.4 Rock slide Schist , strike N - S dip 70 ... flows are common in gneissic rocks whereas rock falls are common in quartzitic rocks . The most affected roads due ...
... flow Burdang slide 30 33.5 Rock - cum- debris slide Rangpo slide 70 40.4 Rock slide Schist , strike N - S dip 70 ... flows are common in gneissic rocks whereas rock falls are common in quartzitic rocks . The most affected roads due ...
Page 69
... flow with interbedded conglomerate in the basal part is widespread and is capped at the top by sediments . The volcanic ... flows ( Fig . 3 ) . Limestone is grey to green coloured and has sharp basal contact . The sandstone is light grey ...
... flow with interbedded conglomerate in the basal part is widespread and is capped at the top by sediments . The volcanic ... flows ( Fig . 3 ) . Limestone is grey to green coloured and has sharp basal contact . The sandstone is light grey ...
Page 155
... flows designated as Panjal Volcanics forming the summit zone of Pir Panjal range . It forms steep scarps . The lava flows are generally light grey and greenish grey to purplish grey in colour , massive , amygdaloidal and highly jointed ...
... flows designated as Panjal Volcanics forming the summit zone of Pir Panjal range . It forms steep scarps . The lava flows are generally light grey and greenish grey to purplish grey in colour , massive , amygdaloidal and highly jointed ...
Contents
CHOUBEY Kewal K Sharma D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
14 other sections not shown
Other editions - View all
Common terms and phrases
02:53 IST MAGNITUDE Accel cm/sē Agglomeratic Slate Amritpur axial plane Bafliaz Formation basin biotite Budhal Burtsa Formation calcite chert clasts conglomerate Cretaceous deformation Dehra Dun deposits dolomite Dum Gali Quartzite facies fault plane feldspar folds foliation fossils Garhwal Geol gneiss grained granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology India Infrakrol Institute of Himalayan inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation Maastrichtian Mandi metamorphic Nappe Nilkanth Panjal thrust Panjal Volcanic Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone Sarkanth schist sector sedimentary sediments sequence shale Sharma shear Shergol Singh SiO2 slide slip slope soil strain Stratigraphy structures Surv Suture Zone Syncline tectonic Tethyan Thakur thick Thinly bedded Uhl valley Unconformity upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Ypresian Zanskar