Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 5
Their correlation is most distinctly observed in the western part of the Central
Pamir ( Fig . 3 ) . The Vanch antiform , composed of Pre - Cambrian rocks ,
overlain by Cambrian , Ordovician and Silurian deposits , is exposed along the
northern ...
Their correlation is most distinctly observed in the western part of the Central
Pamir ( Fig . 3 ) . The Vanch antiform , composed of Pre - Cambrian rocks ,
overlain by Cambrian , Ordovician and Silurian deposits , is exposed along the
northern ...
Page 162
It has been observed that away from the thrusts all the three phases of
deformation are dominant but at or near the thrust faults the third phase of folding
is more prominent than the earlier two phases ( Raj , 1983 ) . Strike slip faults and
normal ...
It has been observed that away from the thrusts all the three phases of
deformation are dominant but at or near the thrust faults the third phase of folding
is more prominent than the earlier two phases ( Raj , 1983 ) . Strike slip faults and
normal ...
Page 211
These results show a pattern of rotational deformation very similar to that
observed in the Palaeogene sediments ( Fig . 1 , Table VII ) . However , the
observed inclinations are much nearer to the present day inclination Cretaceous
and Tertiary ...
These results show a pattern of rotational deformation very similar to that
observed in the Palaeogene sediments ( Fig . 1 , Table VII ) . However , the
observed inclinations are much nearer to the present day inclination Cretaceous
and Tertiary ...
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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