Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
From inside the book
Results 1-3 of 17
Page 54
... later ones . Therefore , in general , the linear fabrics exhibit a triclinic symmetry . Folds : The study of the fold profiles from the present area indicates that the folds are either plane or non - plane . The three dimensional study ...
... later ones . Therefore , in general , the linear fabrics exhibit a triclinic symmetry . Folds : The study of the fold profiles from the present area indicates that the folds are either plane or non - plane . The three dimensional study ...
Page 62
... later stages of D3 deformation the thrust planes were folded . This D3 phase was also responsible for the rotation of F , and F2 folds which is well marked near the thrust zone . Joints were also rotated due to flexural - slip 1 along ...
... later stages of D3 deformation the thrust planes were folded . This D3 phase was also responsible for the rotation of F , and F2 folds which is well marked near the thrust zone . Joints were also rotated due to flexural - slip 1 along ...
Page 171
... later high amplitude signals are likely to be dominated by surface waves , and other phases . One also notices an underlying relatively low frequency signal ( ~ 1-3 Hz ) over which the higher frequency signals are riding . At least in ...
... later high amplitude signals are likely to be dominated by surface waves , and other phases . One also notices an underlying relatively low frequency signal ( ~ 1-3 Hz ) over which the higher frequency signals are riding . At least in ...
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