Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 144
... and the southern edge of the Himalaya is at least 10 mm a . The southward decrease in ages of sediment in the Ganga Basin implies faster convergence , but probably no faster than 20 mm a . The well defined rate of about 10 mm , a at the ...
... and the southern edge of the Himalaya is at least 10 mm a . The southward decrease in ages of sediment in the Ganga Basin implies faster convergence , but probably no faster than 20 mm a . The well defined rate of about 10 mm , a at the ...
Page 149
... to do so would require an estimate of the rate at which material is eroded . ( Modified from Molnar and Lyon - Caen 1988 ) . Journal of Himalayan Geology , Vol . 1 ( 2. Subsidence Uplift له Previous Thrust Fault ? ? ? where ' H ( 10-20 mm / ...
... to do so would require an estimate of the rate at which material is eroded . ( Modified from Molnar and Lyon - Caen 1988 ) . Journal of Himalayan Geology , Vol . 1 ( 2. Subsidence Uplift له Previous Thrust Fault ? ? ? where ' H ( 10-20 mm / ...
Page 150
... to be curved , with steep segments beneath areas of marked increase in elevation and flatter beneath areas of more mature landscape . The rate of convergence between the Indian Shield and the Himalaya is at least 10 mm / a . The average ...
... to be curved , with steep segments beneath areas of marked increase in elevation and flatter beneath areas of more mature landscape . The rate of convergence between the Indian Shield and the Himalaya is at least 10 mm / a . The average ...
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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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