Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 33
It is in this background that the Proterozoic framework of the Indian shield and its
probable extensions would help us to ... to the extension of Sakoli - Sausar
basins ( presently below the trap ) around the southern part of Budelkhand
nucleus ...
It is in this background that the Proterozoic framework of the Indian shield and its
probable extensions would help us to ... to the extension of Sakoli - Sausar
basins ( presently below the trap ) around the southern part of Budelkhand
nucleus ...
Page 214
A marginal basin of undefined extension might have existed in the intervening
area , which was possibly closed later along the present day Shyok zone , north
of the Ladakh Intrusives ( Frank et al . , 1977 ) . The marked drop in northward ...
A marginal basin of undefined extension might have existed in the intervening
area , which was possibly closed later along the present day Shyok zone , north
of the Ladakh Intrusives ( Frank et al . , 1977 ) . The marked drop in northward ...
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 ...
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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