Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 73
... clast , poorly sorted and show inverse to normal grading . Mostly clasts show parallel fabric but at places transverse fabric was also observed . Largest clast measured upto 50 cm and they are self to matrix supported . The conglomerate ...
... clast , poorly sorted and show inverse to normal grading . Mostly clasts show parallel fabric but at places transverse fabric was also observed . Largest clast measured upto 50 cm and they are self to matrix supported . The conglomerate ...
Page 74
... clast ratio 70:30 . Clasts are in general subrounded to subangular and are dominantly of carbonates with few exceptions where volcanic clasts are also present . They are poorly sorted with no preferred orientation . Burtsa Formation ...
... clast ratio 70:30 . Clasts are in general subrounded to subangular and are dominantly of carbonates with few exceptions where volcanic clasts are also present . They are poorly sorted with no preferred orientation . Burtsa Formation ...
Page 87
... clast composition of the conglomerate suggest that these conglomerates are monomict with dominant clast of limestone and dolomite . Occassionaly other clasts such as sandstone and chert ( chert rare ) are also present . Biostratigraphy ...
... clast composition of the conglomerate suggest that these conglomerates are monomict with dominant clast of limestone and dolomite . Occassionaly other clasts such as sandstone and chert ( chert rare ) are also present . Biostratigraphy ...
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/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