Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 63
Space and time distribution of magmatism visa - vis convergence and collision of
the Indian Plate and the Eurasian Plate has been attempted . The magmatic
growth is restricted to two linear belts , ( i ) Indus - Yarlung collision zone and ( ii )
...
Space and time distribution of magmatism visa - vis convergence and collision of
the Indian Plate and the Eurasian Plate has been attempted . The magmatic
growth is restricted to two linear belts , ( i ) Indus - Yarlung collision zone and ( ii )
...
Page 188
Gondwanaland or subsequent , revisions of this reconstruction ( Griffiths , 1974 ;
Norton and Molnar . 1977 ) . In this model the Indus - Tsangpo zone is seen as
the original suture between India and Asia which became inactive after collision
of ...
Gondwanaland or subsequent , revisions of this reconstruction ( Griffiths , 1974 ;
Norton and Molnar . 1977 ) . In this model the Indus - Tsangpo zone is seen as
the original suture between India and Asia which became inactive after collision
of ...
Page 283
The nature and site of initial collision causing this emplacement are disputed . ...
collision between the island - arc and the Indian continent , whereas , same
group of workers elsewhere and others postulate it as an arc and Karakorum belt
...
The nature and site of initial collision causing this emplacement are disputed . ...
collision between the island - arc and the Indian continent , whereas , same
group of workers elsewhere and others postulate it as an arc and Karakorum belt
...
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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