Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 123
The Inner Krol is characterized at the base by the Giri thrust ( = Shali thrust ? ) . It
is interesting to note that these thrusts are possibly concealed below the rocks in
the Garhwal region and hence their analogues have not been reported from the ...
The Inner Krol is characterized at the base by the Giri thrust ( = Shali thrust ? ) . It
is interesting to note that these thrusts are possibly concealed below the rocks in
the Garhwal region and hence their analogues have not been reported from the ...
Page 427
( c ) The pyroxene and platy - gneiss ( unit “ b ” ) of Tibetan slab should be a
synclinal scar , causing the sedimentary series attributable to the base of
Palaeozoic to reappear under a recumbent anticlinal head formed by augen
gneiss ( unit “ c ...
( c ) The pyroxene and platy - gneiss ( unit “ b ” ) of Tibetan slab should be a
synclinal scar , causing the sedimentary series attributable to the base of
Palaeozoic to reappear under a recumbent anticlinal head formed by augen
gneiss ( unit “ c ...
Page 480
Different inetrrelationships among primary sedimentary structures variable
spatially and vertically , strong basal scouring , inverse- to normal - grading at the
base , relatively continuous strata with abrupt pinch - out , occasionally found
within ...
Different inetrrelationships among primary sedimentary structures variable
spatially and vertically , strong basal scouring , inverse- to normal - grading at the
base , relatively continuous strata with abrupt pinch - out , occasionally found
within ...
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Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
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Common terms and phrases
active Asia associated base basement basic basin beds belt biotite blocks Boundary Central collision complex consists continental continuous Cretaceous crust crystalline deformation deposits direction early earthquakes east eastern Eocene et al evolution extension facies faults Figure folds followed formation formed Gansser Garhwal Geol Geology gneiss grade granite Group Higher Himalaya Indian Indian plate indicate Indus initial island Jour Kashmir Ladakh Late Lesser levels limestone Lower magmatic major margin metamorphism Middle mountain movement nappe nature Nepal northern observed occur oceanic ophiolite origin orogenic Pakistan palaeomagnetic Palaeozoic Pande phase plate possible Precambrian present Range region represent rocks rotation sampled sandstones schists sedimentary sediments seismicity sequence Shield similar southern structural studies subduction suggested suture Table tectonic Tertiary Tethyan thickness thrust Tibetan trend units Upper valley volcanics western zone