Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 226
Along the valley and upper slope areas with resistant lithological units , rockfalls
and slides have aided in the development of cliffs . The main valley course of the
Nayar reflects two distinct cycles of erosion thus representing a two cyclic valley ...
Along the valley and upper slope areas with resistant lithological units , rockfalls
and slides have aided in the development of cliffs . The main valley course of the
Nayar reflects two distinct cycles of erosion thus representing a two cyclic valley ...
Page 230
The Satpuli landslide is along the right bank of Eastern Nayar at Satpuli ( Fig . 6d
) where Eastern Nayar undercuts the highly folded and sheared slate , schists
and phyllites of Chandpur and Damta formations . Mostly slides occur towards
the ...
The Satpuli landslide is along the right bank of Eastern Nayar at Satpuli ( Fig . 6d
) where Eastern Nayar undercuts the highly folded and sheared slate , schists
and phyllites of Chandpur and Damta formations . Mostly slides occur towards
the ...
Page 129
The clay mineralogy of < 2 fraction was studied on oriented , glycolated and
heated clay slides by X - ray diffraction . Illite and chlorite are dominant clay
minerals . IM illite was observed in basal and central part of Lingti strata whereas
, IMd ...
The clay mineralogy of < 2 fraction was studied on oriented , glycolated and
heated clay slides by X - ray diffraction . Illite and chlorite are dominant clay
minerals . IM illite was observed in basal and central part of Lingti strata whereas
, IMd ...
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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