Himalaya: geological aspectsContributed 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 are and extend towards the northwest beyond the Hazara-Kashmir
syntaxis. During the period of network observations, the seismicity is mostly
associated with ...
These faults are recognized as basement structures associated with the
Himalayan are and extend towards the northwest beyond the Hazara-Kashmir
syntaxis. During the period of network observations, the seismicity is mostly
associated with ...
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 | 9 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 19 |
Peninsular and Himalayan Precambrian Belts | 31 |
Copyright | |
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Common terms and phrases
Acharyya Alpine Alps associated basement faults basin batholith belt biotite Bordet Central Crystalline collision continental Cretaceous crust crustal deformation deposits Earth Planet earthquakes Eastem Eocene facies field first flow flysch folds foreland formation Gansser Garhwal Geodynamics Geol Geology Geophys geosyncline gneiss Gondwana granite Himalaya Indian plate Indus island arc Jour Karakorum Kashmir Klootwijk Krol Kumaun Ladakh Late Lesser Himalaya limestone lndus Lower magmatic Main Boundary Main Central Thrust margin melange Mesozoic metamorphism Molnar movement nappe Nepal northem occur oceanic ofthe ophiolite orogenic Pakistan Palaeogene palaeomagnetic Palaeozoic Pamir Pande Panjal phase plate tectonics Plateau Precambrian Proterozoic quartzite Quetta Range region rocks rotation Saklani sandstones Saxena schists sedimentary sediments seismicity sequence serpentinite significance Simla Siwalik southem stratigraphic structural subduction Surv suture zone Tectonic Zone Tectonophysics Tertiary Tethyan Tethys thickness Tibetan slab Upper Valdiya volcanics westem
Bibliographic information
| Title | Himalaya: geological aspects Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 15 of Current trends in geology Volume 1 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Author | P. S. Saklani |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Pub. House, 2005 |
| ISBN | 8190228978, 9788190228978 |
| Length | 493 pages |
| Subjects | › › Geology Geology, Structural Metamorphism (Geology) Mountains Science / Earth Sciences / Geology |
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