Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 82
... changes was studied in detail . The detailed petrography of each formation is as follow : Saser Brangsa Formation Carbonates are dominantly micrites and are composed of calcite . In few samples little detritus is present . The detritus ...
... changes was studied in detail . The detailed petrography of each formation is as follow : Saser Brangsa Formation Carbonates are dominantly micrites and are composed of calcite . In few samples little detritus is present . The detritus ...
Page 125
... changes and neotectonic activity in this part of the Himalaya . Acknowledgements : The author expresses his sincere thanks to Dr. V.C. Thakur , Director , Wadia Institute of Himalayan Geology , Dehra Dun for facilities . Sincere thanks ...
... changes and neotectonic activity in this part of the Himalaya . Acknowledgements : The author expresses his sincere thanks to Dr. V.C. Thakur , Director , Wadia Institute of Himalayan Geology , Dehra Dun for facilities . Sincere thanks ...
Page 134
... change in lithotectonic setting on both Table 1. Lithotectonic sequence of the Indus - Tsangpo Suture Zone around ... changes and shear zones . The melange belt is 1 to 4 km wide and exposes the rocks as given in Table 1 . Along the ...
... change in lithotectonic setting on both Table 1. Lithotectonic sequence of the Indus - Tsangpo Suture Zone around ... changes and shear zones . The melange belt is 1 to 4 km wide and exposes the rocks as given in Table 1 . Along the ...
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