Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 12
Page
... granitoids and the migmatites arise from the anatexis of the surrounding metapelites . Compositionally the granitoids range from granodiorite to granite and are peraluminous S - type , corundum normative rocks . They show compositional ...
... granitoids and the migmatites arise from the anatexis of the surrounding metapelites . Compositionally the granitoids range from granodiorite to granite and are peraluminous S - type , corundum normative rocks . They show compositional ...
Page 2
... granitoids occupy mainly the granite field , while the various phases of foliated granitoids , the biotite gneisses and the porphyritic gneisses chemically define compositional range from granodiorite to granite . All the granitoids of ...
... granitoids occupy mainly the granite field , while the various phases of foliated granitoids , the biotite gneisses and the porphyritic gneisses chemically define compositional range from granodiorite to granite . All the granitoids of ...
Page 112
... Granitoids Granitoids are categorised into 7 tectonic environments ( Maniar & Piccoli , 1989 ) . These are island arc granites ( IAG ) , continental arc granites ( CAG ) , continental collision granites ( CCG ) , rift related granites ...
... Granitoids Granitoids are categorised into 7 tectonic environments ( Maniar & Piccoli , 1989 ) . These are island arc granites ( IAG ) , continental arc granites ( CAG ) , continental collision granites ( CCG ) , rift related granites ...
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