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Page 112
Collision orogens seemingly still weaker in foreland tectonisation may be
exemplified by the superficially deformed Zagros Range. However, this range
has recently been understood more fully as underlain, beneath its decollement
cover, by a ...
Collision orogens seemingly still weaker in foreland tectonisation may be
exemplified by the superficially deformed Zagros Range. However, this range
has recently been understood more fully as underlain, beneath its decollement
cover, by a ...
Page 189
South of the lndus-Tsangpo suture zone, the lndiaAsia collision has resulted in
large scale peninsular verging thrusting of the more exterior zones of continental
lndo-Pakistan. In the West (i.e. eastem Baluchistan and the Salt Range-Potwar ...
South of the lndus-Tsangpo suture zone, the lndiaAsia collision has resulted in
large scale peninsular verging thrusting of the more exterior zones of continental
lndo-Pakistan. In the West (i.e. eastem Baluchistan and the Salt Range-Potwar ...
Page 192
Crawford (l974c) suggested that the Salt Range - Potwar Plateau unit was
formerly in line with the main Himalayan front and that this unit has rotated over
about 70 degrees counterclockwise around a pole near the eastem end of the
Salt ...
Crawford (l974c) suggested that the Salt Range - Potwar Plateau unit was
formerly in line with the main Himalayan front and that this unit has rotated over
about 70 degrees counterclockwise around a pole near the eastem end of the
Salt ...
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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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