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Page 112
In a mountain complex structured alter 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 alter 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 188
In this model the Indus-Tsangpo zone is seen as the original suture between
India and Asia which became inactive alter collision of the two continental blocks
(pre-Middle Eocene). ln post-Oligocene times renewed convergence
commenced ...
In this model the Indus-Tsangpo zone is seen as the original suture between
India and Asia which became inactive alter collision of the two continental blocks
(pre-Middle Eocene). ln post-Oligocene times renewed convergence
commenced ...
Page 283
The nature and site of initial collision causing this emplacement are disputed.
Reynolds et al. (1983), Jan and Asif( 1983) consider this as a collision between
the island-are and the Indian continent, whereas, same group of workers
elsewhere ...
The nature and site of initial collision causing this emplacement are disputed.
Reynolds et al. (1983), Jan and Asif( 1983) consider this as a collision between
the island-are and the Indian continent, whereas, same group of workers
elsewhere ...
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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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