Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 11
Page 133
... melange of the Indus Suture Zone reveals that there is no distinctive shape of strain ellipsoid . Majority of the pebbles of limestone , slate and serpentine are triaxial flattening type ellipsoids , while pebbles of argillaceous ...
... melange of the Indus Suture Zone reveals that there is no distinctive shape of strain ellipsoid . Majority of the pebbles of limestone , slate and serpentine are triaxial flattening type ellipsoids , while pebbles of argillaceous ...
Page 134
... Zone around Shergol . -Zanskar Thrust Table 2. Es and U values of pebbles of different. 1981 , 1990 ) . A separate lithostratigraphic unit of the Nindam Formation lies between two ophiolitic melange belts . The Nindam Formation is of ...
... Zone around Shergol . -Zanskar Thrust Table 2. Es and U values of pebbles of different. 1981 , 1990 ) . A separate lithostratigraphic unit of the Nindam Formation lies between two ophiolitic melange belts . The Nindam Formation is of ...
Page 137
... Zone , Ladakh , J & K. 1. Dras- Naktul volcanoclastics and flysch , 2. Pillow lavas , sills and dyke series , 3. Ultramafic lenses . Melange Unit : 4. Shergol Conglomerate : 5. Melange formation , 6 . Shergol blueschist zone . Higher ...
... Zone , Ladakh , J & K. 1. Dras- Naktul volcanoclastics and flysch , 2. Pillow lavas , sills and dyke series , 3. Ultramafic lenses . Melange Unit : 4. Shergol Conglomerate : 5. Melange formation , 6 . Shergol blueschist zone . Higher ...
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/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