Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 46
These sediments represent flyschoidal to continental slope followed by outer to
inner shelf depositional environment upto Middle Cambrian . The Late Cambrian
represents shallow shallow marine environment culminating into tidal flat ...
These sediments represent flyschoidal to continental slope followed by outer to
inner shelf depositional environment upto Middle Cambrian . The Late Cambrian
represents shallow shallow marine environment culminating into tidal flat ...
Page 261
This tectonostratigraphic arrangement clearly represents migration of a site on
the oceanic lithosphere from basinal ... The presence of several shear zones and
NE trending slickensides and polished surfaces of different blocks represent a ...
This tectonostratigraphic arrangement clearly represents migration of a site on
the oceanic lithosphere from basinal ... The presence of several shear zones and
NE trending slickensides and polished surfaces of different blocks represent a ...
Page 20
Dots on the diagram represent individual plagioclases from the Panjal Trap of
Bandipura. JB. Bivariate diagram showing the relationship of 2 Q peak positions
of l3I reflections and the anorlhite content of the plagioelases (Bambauer e! al.
Dots on the diagram represent individual plagioclases from the Panjal Trap of
Bandipura. JB. Bivariate diagram showing the relationship of 2 Q peak positions
of l3I reflections and the anorlhite content of the plagioelases (Bambauer e! al.
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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