Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 23
Page 52
... developed coaxially on the limbs of F , fold . F , is chevron fold with axial plane ( S , ) developed on the limb of F , fold and the hinge lie at steep angle to F , and F2 folds . The intersection of bedding plane ( S , ) and axial ...
... developed coaxially on the limbs of F , fold . F , is chevron fold with axial plane ( S , ) developed on the limb of F , fold and the hinge lie at steep angle to F , and F2 folds . The intersection of bedding plane ( S , ) and axial ...
Page 62
... developed during D , phase of deformation . The second generation of axial plane ( S ) developed on F2 folds . This phase of deformation was also responsible for the formation of second generation of linear fabrics such as crenulation ...
... developed during D , phase of deformation . The second generation of axial plane ( S ) developed on F2 folds . This phase of deformation was also responsible for the formation of second generation of linear fabrics such as crenulation ...
Page 81
... developed along the border of plagioclase having contact with the K - feldspar . Plagioclase is the dominanting mineral of this rock and varies in composition from oligoclase to andesine . It shows a variety of zoning and twinning ...
... developed along the border of plagioclase having contact with the K - feldspar . Plagioclase is the dominanting mineral of this rock and varies in composition from oligoclase to andesine . It shows a variety of zoning and twinning ...
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