Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 15
... flow along the trace of the SKZ ( Fig . 1 ) . There are no peaks above 6000 m in the Tethyan zone to the west of PMZ ... flows due NW . This is possibly due to neotectonic movements in the Kishtwar region along the SKZ . over the ...
... flow along the trace of the SKZ ( Fig . 1 ) . There are no peaks above 6000 m in the Tethyan zone to the west of PMZ ... flows due NW . This is possibly due to neotectonic movements in the Kishtwar region along the SKZ . over the ...
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 ° Easterly Quartzite & phyllite , strike NW - SE dip 55 ° NE Highly weathered formation , heavy precipitation , sinking ...
... flow Burdang slide 30 33.5 Rock - cum- debris slide Rangpo slide 70 40.4 Rock slide Schist , strike N - S dip 70 ° Easterly Quartzite & phyllite , strike NW - SE dip 55 ° NE Highly weathered formation , heavy precipitation , sinking ...
Page 69
... flow vary in thickness from 20 to 300 m ( approx . ) from east to west . The overlying sedimentaries include ... flows ( Fig . 3 ) . Limestone is grey to green coloured and has sharp basal contact . The sandstone is light grey , fine Fig ...
... flow vary in thickness from 20 to 300 m ( approx . ) from east to west . The overlying sedimentaries include ... flows ( Fig . 3 ) . Limestone is grey to green coloured and has sharp basal contact . The sandstone is light grey , fine Fig ...
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 |
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02:53 IST MAGNITUDE Accel cm/s² 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