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Page 421
The MCT represents a transition zone between the kyanite-gneiss and the gamet
bearing phyllite with altemating bands of quartzites, marbles, amphibolites and
augen gneiss of the Scale zone. It corresponds probably to a major surface of ...
The MCT represents a transition zone between the kyanite-gneiss and the gamet
bearing phyllite with altemating bands of quartzites, marbles, amphibolites and
augen gneiss of the Scale zone. It corresponds probably to a major surface of ...
Page 422
The injection of leucogranite took place in a sheared surface similar to that of the
Central Nepal, but located downwards into the platy-gneiss. It is the granite which
was responsible for the development of the huge recumbent fold of Everest, It, ...
The injection of leucogranite took place in a sheared surface similar to that of the
Central Nepal, but located downwards into the platy-gneiss. It is the granite which
was responsible for the development of the huge recumbent fold of Everest, It, ...
Page 424
(i) The stratigraphic interpretation: It the extrapolation towards the east of what
was accepted for Ulleri gneiss. But the gigantic dimensions of Arun gneiss
completely differ from those of the Ulleri gneiss, and hence such an extrapolation
should ...
(i) The stratigraphic interpretation: It the extrapolation towards the east of what
was accepted for Ulleri gneiss. But the gigantic dimensions of Arun gneiss
completely differ from those of the Ulleri gneiss, and hence such an extrapolation
should ...
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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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