Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 51
... surfaces and show displacement normal to the joint surface . Normally the tension joints cut across the bedding planes ( S1 ) or schistosity ( S ) at a high angle which decreases with progressive shearing . Mostly the tention joints are ...
... surfaces and show displacement normal to the joint surface . Normally the tension joints cut across the bedding planes ( S1 ) or schistosity ( S ) at a high angle which decreases with progressive shearing . Mostly the tention joints are ...
Page 52
... surfaces with the axial planes of different generations of folds . In the folded rocks this lineation is produced by the intersection of the axial planes with the folded surface . With the increase in the number of S - surfaces the ...
... surfaces with the axial planes of different generations of folds . In the folded rocks this lineation is produced by the intersection of the axial planes with the folded surface . With the increase in the number of S - surfaces the ...
Page 180
... surface integral over the fault plane F. Since the integrand involves delta functions the surface integrals reduce to line integrals and th ( xy ) = t These are known as the = ah ar ( x , y ) t isochrone curves . Thus the surface ...
... surface integral over the fault plane F. Since the integrand involves delta functions the surface integrals reduce to line integrals and th ( xy ) = t These are known as the = ah ar ( x , y ) t isochrone curves . Thus the surface ...
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