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 132
Farther north , the ancient southern edge of southern Asia is defined by the
Kangdese granites and overlying sedimentary rock . ( This cross section is
derived largely from Gansser's ( 1964 ) , and is modified from Molnar's [ 1984 ]
simplified ...
Farther north , the ancient southern edge of southern Asia is defined by the
Kangdese granites and overlying sedimentary rock . ( This cross section is
derived largely from Gansser's ( 1964 ) , and is modified from Molnar's [ 1984 ]
simplified ...
Page 141
APPROXIMATE SOUTHERN MARGIN OF THE INDO - GANGETIC PLAINS 100
200 km DELMI o & CENTRA TIC Geologic constraints on rates of convergence
between the Indian shield and the Himalaya At present , the only estimates of
rates ...
APPROXIMATE SOUTHERN MARGIN OF THE INDO - GANGETIC PLAINS 100
200 km DELMI o & CENTRA TIC Geologic constraints on rates of convergence
between the Indian shield and the Himalaya At present , the only estimates of
rates ...
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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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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