Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 159
Printed in India Sedimentological Studies of the Upper Siwalik Boulder
Conglomerate Formation , Mohand Area , District Saharanpur , U.P. ROHTASH
KUMAR & SUMIT K. GHOSH Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
Printed in India Sedimentological Studies of the Upper Siwalik Boulder
Conglomerate Formation , Mohand Area , District Saharanpur , U.P. ROHTASH
KUMAR & SUMIT K. GHOSH Wadia Institute of Himalayan Geology , Dehra Dun -
248001 ...
Page 163
The Upper Siwalik Conglomerate bed shows almost same variance range in
other sectors ( Tandon , 1976 ; Parkash , et al . , 1974 ; Kumar & Tandon , 1985 ) .
The high variance value in the Upper Siwalik Conglomerate is possibly because
of ...
The Upper Siwalik Conglomerate bed shows almost same variance range in
other sectors ( Tandon , 1976 ; Parkash , et al . , 1974 ; Kumar & Tandon , 1985 ) .
The high variance value in the Upper Siwalik Conglomerate is possibly because
of ...
Page 166
In the Upper Siwalik Boulder Conglomerate , the Tal Formation has contributed >
30 % clasts , in which siliciclastic clasts are prominent ( 15-20 % ) . The size of
the siliciclastic clasts ranges from 10-40 cm . The other clasts of the Tal Formation
...
In the Upper Siwalik Boulder Conglomerate , the Tal Formation has contributed >
30 % clasts , in which siliciclastic clasts are prominent ( 15-20 % ) . The size of
the siliciclastic clasts ranges from 10-40 cm . The other clasts of the Tal Formation
...
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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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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