Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 28
... present authors ) and the southern unit . ( Ramban Group of the present authors ) were considered to be stratigraphically and structurally discontinuous by some workers and the Banihal- Ramban area is shown to be constituted of two or ...
... present authors ) and the southern unit . ( Ramban Group of the present authors ) were considered to be stratigraphically and structurally discontinuous by some workers and the Banihal- Ramban area is shown to be constituted of two or ...
Page 28
... present authors ) and the southern unit ( Ramban Group of the present authors ) were considered to be stratigraphically and structurally discontinuous by some workers and the BanihalRamban area is shown to be constituted of two or three ...
... present authors ) and the southern unit ( Ramban Group of the present authors ) were considered to be stratigraphically and structurally discontinuous by some workers and the BanihalRamban area is shown to be constituted of two or three ...
Page 194
... present snout confirms the retreating nature of the glacier in present times . The lateral static moraines on both sides of the glacier are the remanants of past glaciations . At a later stage glacial advance was restricted between ...
... present snout confirms the retreating nature of the glacier in present times . The lateral static moraines on both sides of the glacier are the remanants of past glaciations . At a later stage glacial advance was restricted between ...
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