Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 101
Chingchang ABSTRACT The Himalaya and the Alps are collision - produced
mountain - belts bordering a part of the Eurasian Plate , which is underridden by
the Indian Plate in the former belt and overridden by the African in the latter .
Chingchang ABSTRACT The Himalaya and the Alps are collision - produced
mountain - belts bordering a part of the Eurasian Plate , which is underridden by
the Indian Plate in the former belt and overridden by the African in the latter .
Page 112
In a mountain complex structured after this particular style , the impedence
caused by the collision is diffused on the passive foreland to result in a wide zone
of deformation , in which the subsequent intra - plate subductions are performed
as ...
In a mountain complex structured after this particular style , the impedence
caused by the collision is diffused on the passive foreland to result in a wide zone
of deformation , in which the subsequent intra - plate subductions are performed
as ...
Page 113
The Alpine mountain belt is still distinguishable into a number of preorogenic and
/ or synorogenic troughs and cordilleras . On the contrary , the Himalaya ,
representing a more advanced stage of mountain building along a convergent
plate ...
The Alpine mountain belt is still distinguishable into a number of preorogenic and
/ or synorogenic troughs and cordilleras . On the contrary , the Himalaya ,
representing a more advanced stage of mountain building along a convergent
plate ...
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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