Himalaya: Geological Aspects, Volume 1Contributed articles. |
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Page 51
The narrowing of the root zone is associated with the disappearance of the varied
styles of its central part and with the interpenetration of marginal styles , i.e. the
induced fold style with imbrication . A narrow imbrication zone being associated ...
The narrowing of the root zone is associated with the disappearance of the varied
styles of its central part and with the interpenetration of marginal styles , i.e. the
induced fold style with imbrication . A narrow imbrication zone being associated ...
Page 229
These faults are recognized as basement structures associated with the
Himalayan arc and extend towards the northwest beyond the Hazara - Kashmir
syntaxis . During the period of network observations , the seismicity is mostly
associated ...
These faults are recognized as basement structures associated with the
Himalayan arc and extend towards the northwest beyond the Hazara - Kashmir
syntaxis . During the period of network observations , the seismicity is mostly
associated ...
Page 240
associated with relatively continuous seismic activity . However , the maximum
magnitude associated with rupture of the Basement Thrust is considerably
smaller than the magnitudes of the great earthquakes on the Detachment .
Aseismic slip ...
associated with relatively continuous seismic activity . However , the maximum
magnitude associated with rupture of the Basement Thrust is considerably
smaller than the magnitudes of the great earthquakes on the Detachment .
Aseismic slip ...
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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