Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 3
Page 6
... production in the crust . Earth Planet . Sci . Lett . , 86 , 287-306 . CONDIE , K.C. , 1973. Archean magmatism and crustal thickening . Geol . Soc . America Bull . , 84 , 2981-2992 . DAS , B.K. & RASTOGI , R. , 1978. Evidence of contact ...
... production in the crust . Earth Planet . Sci . Lett . , 86 , 287-306 . CONDIE , K.C. , 1973. Archean magmatism and crustal thickening . Geol . Soc . America Bull . , 84 , 2981-2992 . DAS , B.K. & RASTOGI , R. , 1978. Evidence of contact ...
Page 42
... produce heterogenous soil mass . In case of rock - cum - debris slides , gneissic rocks show a higher incidence of landslides as compared to others . This is due to the fact that gneisses are massive in nature in Sikkim Himalaya and ...
... produce heterogenous soil mass . In case of rock - cum - debris slides , gneissic rocks show a higher incidence of landslides as compared to others . This is due to the fact that gneisses are massive in nature in Sikkim Himalaya and ...
Page 57
... produce a sub - parallel to parallel pattern of the dip isogon and belong to class 2. Such type of class 2 folds are similar folds and thus , suggest a slip mechanism for the origin of these folds ( Ramsay , 1967 ) . Dip isogon , with ...
... produce a sub - parallel to parallel pattern of the dip isogon and belong to class 2. Such type of class 2 folds are similar folds and thus , suggest a slip mechanism for the origin of these folds ( Ramsay , 1967 ) . Dip isogon , with ...
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