Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 129
... mineral grains ) where with cessation of stress the antimony and associated minerals formed as hydrothermal deposits ( secondary ) ; and the stibnite / metastibnite due to the process of oxidation has been further transformed into ...
... mineral grains ) where with cessation of stress the antimony and associated minerals formed as hydrothermal deposits ( secondary ) ; and the stibnite / metastibnite due to the process of oxidation has been further transformed into ...
Page 129
... mineral grains ) where with cessation of stress the antimony and associated minerals formed as hydrothermal deposits ( secondary ) ; and the stibnite / metastibnite due to the process of oxidation has been further transformed into ...
... mineral grains ) where with cessation of stress the antimony and associated minerals formed as hydrothermal deposits ( secondary ) ; and the stibnite / metastibnite due to the process of oxidation has been further transformed into ...
Page 173
... minerals are crystallized . The first phase of deformation ( D ) represents the first phase of upheaval of Himalaya . It involved large scale of folding of bedding plane ( So ) , resulted in the development of isoclinal mesoscopic folds ...
... minerals are crystallized . The first phase of deformation ( D ) represents the first phase of upheaval of Himalaya . It involved large scale of folding of bedding plane ( So ) , resulted in the development of isoclinal mesoscopic folds ...
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