Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 108
Correlation by Srikantia and Sharma ( 1972 ) of the salt horizons of Mandi with
the Salt Range thus becomes redundant since they correlate the Khewra
Formation of Lower Cambrian age with Khaira Member and also the Shali
sequence with ...
Correlation by Srikantia and Sharma ( 1972 ) of the salt horizons of Mandi with
the Salt Range thus becomes redundant since they correlate the Khewra
Formation of Lower Cambrian age with Khaira Member and also the Shali
sequence with ...
Page 165
The microphone is in the lower block , approximately 2 cm from the fault , in the
vicinity of the accelerometers . The digital waveforms are analyzed for indications
of tensional motion , i.e. , motion normal to the fault plane . Figure 6 shows some
...
The microphone is in the lower block , approximately 2 cm from the fault , in the
vicinity of the accelerometers . The digital waveforms are analyzed for indications
of tensional motion , i.e. , motion normal to the fault plane . Figure 6 shows some
...
Page 191
The Siwalik belt comprises predominantly the rocks belonging to the Siwalik
Group , which on the basis of lithological characteristics and associations , is
divisible into ( 1 ) Lower Siwalik , ( 2 ) Middle Siwalik and ( 3 ) Upper Siwalik .
The Siwalik belt comprises predominantly the rocks belonging to the Siwalik
Group , which on the basis of lithological characteristics and associations , is
divisible into ( 1 ) Lower Siwalik , ( 2 ) Middle Siwalik and ( 3 ) Upper Siwalik .
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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