Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 131
Nevertheless , geomorphic observations suggest that the rock of the Greater
Himalaya may rise more rapidly than that of the Lesser Himalaya , except at the
southern front of the Lesser Himalaya . Both geodetic measurements and folding
and ...
Nevertheless , geomorphic observations suggest that the rock of the Greater
Himalaya may rise more rapidly than that of the Lesser Himalaya , except at the
southern front of the Lesser Himalaya . Both geodetic measurements and folding
and ...
Page 148
The evidence reported above suggests relatively rapid vertical speeds of material
both in the Greater Himalaya and at the ... In addition , two quantitative
observations suggest that erosion rates in the Lesser Himalaya are lower than
those in ...
The evidence reported above suggests relatively rapid vertical speeds of material
both in the Greater Himalaya and at the ... In addition , two quantitative
observations suggest that erosion rates in the Lesser Himalaya are lower than
those in ...
Page 254
Values 1.5-2.5 suggest a crystal fractionation model with olivine and plagioclase
as the fractionating phases ( see Francis et al . , 1983 ) . Therefore , the data
suggests an additional fractionating phase in the dolerite rocks . Relatively flat ...
Values 1.5-2.5 suggest a crystal fractionation model with olivine and plagioclase
as the fractionating phases ( see Francis et al . , 1983 ) . Therefore , the data
suggests an additional fractionating phase in the dolerite rocks . Relatively flat ...
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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 |
28 other sections not shown
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Common terms and phrases
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