Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 103
103-114 . Printed in India Vendian - Lower Cambrian desiccation along the
Southern Margin of the Proto - Tethys N. S. VIRDI Wadia Institute of Himalayan
Geology , Dehra Dun - 248001 , India Abstract : Widespread salt and evaporite
bearing ...
103-114 . Printed in India Vendian - Lower Cambrian desiccation along the
Southern Margin of the Proto - Tethys N. S. VIRDI Wadia Institute of Himalayan
Geology , Dehra Dun - 248001 , India Abstract : Widespread salt and evaporite
bearing ...
Page 111
We can thus compare the northern margin of the Gondwanaland in the Indian
subcontinent to an Atlantic type passive ... The distribution of the evaporites along
passive margins is also controlled by the orientation of the margins vis - a - vis
the ...
We can thus compare the northern margin of the Gondwanaland in the Indian
subcontinent to an Atlantic type passive ... The distribution of the evaporites along
passive margins is also controlled by the orientation of the margins vis - a - vis
the ...
Page 112
However the margin behaved as a convergent margin during its later
evolutionary history and thus the identification of transforms or other pre -
collision structures is not so easy . Stocklin ( 1986 ) has proposed that a major
tectonic feature the ...
However the margin behaved as a convergent margin during its later
evolutionary history and thus the identification of transforms or other pre -
collision structures is not so easy . Stocklin ( 1986 ) has proposed that a major
tectonic feature the ...
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Contents
The Shyok valley Northern Ladakh India An entraped and compressed marginal | 1 |
Chemical mineralogy of the Panjal Traps around Bandipura Kashmir | 17 |
Structural characteristics of the rocks of BanihalRamban area | 23 |
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activity associated authors basin beds belt biotite block Central correlation Crystallines deformation deposits developed District dolerite earthquakes eastern et al event exposed extends facies fault feldspars field folds followed Formation formed Garhwal Geol Geology gneisses grade grains granite granitoids Group higher Himalaya Himalayan Geology hornblende India indicate Indus Institute Jour Krol Ladakh Late later Lesser Himalaya limestone lower Main major margin material metamorphism Middle minerals nature Nayar northern observed occur oceanic ophiolitic origin phase phyllite plagioclase plane plate Pradesh present quartz quartzite range References region represented result river rocks Salt samples sandstone schist sedimentary sediments sequence Series shale Sharma Shyok Siwalik slip slope southern Spiti structural Subathu subduction suggests surface Suture Table tectonic thick Thrust trend units Upper valley values variation volcanics Wadia western zone