Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 17
Deformation D : Folds of D , generation are overturned isoclinal folds of all sizes ,
folding the preHimalayan lithic banding or metamorphic layering . D folds ,
trending NW - SE , plunge due NW at low angles of about 10 to 12 degrees . D ,
folds ...
Deformation D : Folds of D , generation are overturned isoclinal folds of all sizes ,
folding the preHimalayan lithic banding or metamorphic layering . D folds ,
trending NW - SE , plunge due NW at low angles of about 10 to 12 degrees . D ,
folds ...
Page 178
On the scale of the area the hinge lines of different phases of folds are nearly
coaxial . However , locally the hinge line of earlier folds show variation in their
direction and amount of plunge due to refolding . The variations in the direction
and ...
On the scale of the area the hinge lines of different phases of folds are nearly
coaxial . However , locally the hinge line of earlier folds show variation in their
direction and amount of plunge due to refolding . The variations in the direction
and ...
Page 186
C. Photograph of phyllite from southeast of Khola village showing open
concentric fold of first generation ( Fi ) . D. Photograph of phyllite from southeast
of Khola showing closed type of similar folds of second generation . 186 Journal
of ...
C. Photograph of phyllite from southeast of Khola village showing open
concentric fold of first generation ( Fi ) . D. Photograph of phyllite from southeast
of Khola showing closed type of similar folds of second generation . 186 Journal
of ...
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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