Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 71
... strain calculation . The center - to - center technique is applied for the calculation of finite strain . The strain in this zone shows two trends correlatable with two penetrative deformation episodes : ( a ) a general increase in the ...
... strain calculation . The center - to - center technique is applied for the calculation of finite strain . The strain in this zone shows two trends correlatable with two penetrative deformation episodes : ( a ) a general increase in the ...
Page 74
Finite Strain in the Berinag Thrust Sheet Strain Marker and Methodology The rocks of the Berinag Thrust Sheet are rich in quartz which varies from 80 to 98 per cent in the schistose quartzite . It is difficult to measure accurately the ...
Finite Strain in the Berinag Thrust Sheet Strain Marker and Methodology The rocks of the Berinag Thrust Sheet are rich in quartz which varies from 80 to 98 per cent in the schistose quartzite . It is difficult to measure accurately the ...
Page 77
... strain values . The strain values have gone upto 3.8 1.8 1 and is interpreted as representing the cummulative strain incorporated first by MCT and later by crystallines thrusting in coaxial fashion over the Lesser Himalaya . The author ...
... strain values . The strain values have gone upto 3.8 1.8 1 and is interpreted as representing the cummulative strain incorporated first by MCT and later by crystallines thrusting in coaxial fashion over the Lesser Himalaya . The author ...
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