Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 74
... associated with limestone and is traversed by calcite veins . Shale in lower part is 150 m thick and is associated with fine grained , thinly bedded sandstone . Shale is generally dark grey to black coloured , fissile and highly cleaved ...
... associated with limestone and is traversed by calcite veins . Shale in lower part is 150 m thick and is associated with fine grained , thinly bedded sandstone . Shale is generally dark grey to black coloured , fissile and highly cleaved ...
Page 75
... associated with limestone and recur at various stratigraphic levels . Cherty limestone is cream coloured and is restricted in some horizons . In the upper part , limestone and fossiliferous limestone with subordinate sandstone is associated ...
... associated with limestone and recur at various stratigraphic levels . Cherty limestone is cream coloured and is restricted in some horizons . In the upper part , limestone and fossiliferous limestone with subordinate sandstone is associated ...
Page 102
... associated with oceanic eddies have been extensively studied to tackle energy and food problems . Problems associated with natural hazards like cyclones , sea level changes , earth quakes need to be also tackled , on priority basis . In ...
... associated with oceanic eddies have been extensively studied to tackle energy and food problems . Problems associated with natural hazards like cyclones , sea level changes , earth quakes need to be also tackled , on priority basis . 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 |
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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