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Page 111
On account of this, the Main Central Thrust, became no longer open as a
passage down to the mantle level. lt was replaced in turn by the more external
Main Boundary Fault since Pliocene time. The Main Boundary Fault provided a
new ...
On account of this, the Main Central Thrust, became no longer open as a
passage down to the mantle level. lt was replaced in turn by the more external
Main Boundary Fault since Pliocene time. The Main Boundary Fault provided a
new ...
Page 338
In Kashmir no thrust equivalent in magnitude or extension to the Main Central
Thrust exists. The Main Boundary Fault itselfis split into two major faults viz. the
so called Main Boundary Fault (Middlemiss, l9 l 9; Wadia, 1928; J ammu Fault of
...
In Kashmir no thrust equivalent in magnitude or extension to the Main Central
Thrust exists. The Main Boundary Fault itselfis split into two major faults viz. the
so called Main Boundary Fault (Middlemiss, l9 l 9; Wadia, 1928; J ammu Fault of
...
Page 411
STRUCTURAL CHARACTERS A cross section from south to north reveals
Nepalese and Nepal nappe Series bordered by Main Boundary Thrust and
further to the north, the Tibetan Series are bounded by Main Central Thrust. The
Nepalese ...
STRUCTURAL CHARACTERS A cross section from south to north reveals
Nepalese and Nepal nappe Series bordered by Main Boundary Thrust and
further to the north, the Tibetan Series are bounded by Main Central Thrust. The
Nepalese ...
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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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