Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 185
Extrapolation of this palaeomagnetically established collision sequence to other
regions along the Indus - Tsangpo suture zone is not possible as yet . After
intimate collision , continued northward movement of continental Indo - Pakistan
...
Extrapolation of this palaeomagnetically established collision sequence to other
regions along the Indus - Tsangpo suture zone is not possible as yet . After
intimate collision , continued northward movement of continental Indo - Pakistan
...
Page 214
These observations do not favour possible formation of the proposed marginal
basin through extensive back arc spreading , as found in present day marginal
basins around the Pacific ( Karig , 1970 , 1971a , 1971b ; Chase , 1978 ) .
Collision ...
These observations do not favour possible formation of the proposed marginal
basin through extensive back arc spreading , as found in present day marginal
basins around the Pacific ( Karig , 1970 , 1971a , 1971b ; Chase , 1978 ) .
Collision ...
Page 242
First motions from this seismicity are consistent with reverse slip on such a fault ,
NE side up , but a large component of left - lateral strike - slip is also possible . In
analogy with the tectonic framework in northern Pakistan , Armbruster et al .
First motions from this seismicity are consistent with reverse slip on such a fault ,
NE side up , but a large component of left - lateral strike - slip is also possible . In
analogy with the tectonic framework in northern Pakistan , Armbruster et al .
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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