Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 46
... represent flyschoidal to continental slope followed by outer to inner shelf depositional environment upto Middle Cambrian . The Late Cambrian represents shallow marine environment culminating into tidal flat complex . Conglomerate ...
... represent flyschoidal to continental slope followed by outer to inner shelf depositional environment upto Middle Cambrian . The Late Cambrian represents shallow marine environment culminating into tidal flat complex . Conglomerate ...
Page 46
... represented by tidal flat complex followed by shelf sedimentation . The polymictite , mudstone and sandstone facies ( Ganmachidam Formation ) developed in certain parts on the Po Formation and they represent debris flow deposits . The ...
... represented by tidal flat complex followed by shelf sedimentation . The polymictite , mudstone and sandstone facies ( Ganmachidam Formation ) developed in certain parts on the Po Formation and they represent debris flow deposits . The ...
Page 196
... represent the basal part of the Tethyan rock sequences . If this conjecture happens to be true , then the Tuting - Tidding belt which occurs to north of the Se La belt may represent a suture zone , very well comparable with the Indus ...
... represent the basal part of the Tethyan rock sequences . If this conjecture happens to be true , then the Tuting - Tidding belt which occurs to north of the Se La belt may represent a suture zone , very well comparable with the Indus ...
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