Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 417
At its upper interface , the Tibetan slab is overlain by the thick pile of Tibetan
series of folded Palaeozoic and Mesozoic sediments ( 10000m ) ( Fuchs , 1968 ;
Fuchs and Frank , 1970 ; Frank and Fuchs , 1970 ; Bordet , 1961 , 1970 , 1973 ,
1975 ...
At its upper interface , the Tibetan slab is overlain by the thick pile of Tibetan
series of folded Palaeozoic and Mesozoic sediments ( 10000m ) ( Fuchs , 1968 ;
Fuchs and Frank , 1970 ; Frank and Fuchs , 1970 ; Bordet , 1961 , 1970 , 1973 ,
1975 ...
Page 425
In this case , the Tibetan slab should extend for 100 km or more , southwards of
the present exposition of the MCT . The westwards extension of Tibetan slab It is
sure that the Tibetan slab extends not only in Nepal , but beyond the India -
Nepal ...
In this case , the Tibetan slab should extend for 100 km or more , southwards of
the present exposition of the MCT . The westwards extension of Tibetan slab It is
sure that the Tibetan slab extends not only in Nepal , but beyond the India -
Nepal ...
Page 426
Further west , valdiya ( 1964 ) described the MCT and the Tibetan slab in the
Pithoragarh and Nanda Devi areas . Unit “ a ” belonging to the Tibetan slab is
also typically exposed in the source region of the Ganga ( Colchen and Le Fort ...
Further west , valdiya ( 1964 ) described the MCT and the Tibetan slab in the
Pithoragarh and Nanda Devi areas . Unit “ a ” belonging to the Tibetan slab is
also typically exposed in the source region of the Ganga ( Colchen and Le Fort ...
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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