Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 33
... period of quiescence . Abundant sand facies corresponds to a higher rate of subsidence than the infilling rate . Fig . 7. Block diagram explaining variation in the depositional environment of the Upper Siwalik Sub - group through ...
... period of quiescence . Abundant sand facies corresponds to a higher rate of subsidence than the infilling rate . Fig . 7. Block diagram explaining variation in the depositional environment of the Upper Siwalik Sub - group through ...
Page 46
... period ( Fig . 3 ) . Conclusion An overview of the above discussed detailed lithostratigraphy , facies variation and field characters suggest the following : The Cambrian was dominated by sandstone facies followed by mudstone and ...
... period ( Fig . 3 ) . Conclusion An overview of the above discussed detailed lithostratigraphy , facies variation and field characters suggest the following : The Cambrian was dominated by sandstone facies followed by mudstone and ...
Page 46
... period ( Fig . 3 ) . Conclusion accumulation followed by tidal flat complex and inner shelf depositional environment is envisaged . Carboniferous was period of varied sedimentation with complex array of facies , depositional environment ...
... period ( Fig . 3 ) . Conclusion accumulation followed by tidal flat complex and inner shelf depositional environment is envisaged . Carboniferous was period of varied sedimentation with complex array of facies , depositional environment ...
Contents
RAJESH SHARMA B K NAYAK Ore petrology and origin of leadzinc deposits in great limestone | 103 |
R K MAZARI T N BAGATI Postcollision graben development in the Spiti valley Himachal | 111 |
P Dobhal SURENDAR KUMAR A K MUNDEPI Mass wasting and slope analysis of Chhota | 119 |
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Common terms and phrases
amphibolite Amritpur Amritpur Granite basin beds biotite block chlorite clasts conglomerate Cretaceous Crystallines deformation deposits developed dolerite dolomite earthquakes eastern Eocene evaporites facies fault feldspars folds fossils Garhwal Garhwal Himalaya garnet Geol glacial glacier gneisses Gondwana grained granitoids Group Himachal Pradesh Himalaya Himalayan Geology hornblende hornblende schists India Indian plate indicate Indus Suture Institute of Himalayan Jour Journal of Himalayan K-feldspar Krol Belt Kumar Kumaun Ladakh Lesser Himalaya limestone lineaments lithology lower magmatic margin metamorphism Middle Siwalik migmatites minerals Molnar moraines muscovite Nayar observed occur ophiolitic Ophiolitic Melange Pakistan phase phyllite plagioclase plane Precambrian quartz quartzite Rawat region river rocks Salt Range samples sandstone schist sedimentary sediments sequence shale Sharma shear zones shows Shyok Singh Siwalik slope Spiti stratigraphic structure Subathu Subathu Formation subduction Surv Suture Zone syncline tectonic Tethyan Thakur thick Thrust trend Upper Siwalik valley volcanics Wadia Institute western Zanskar