Himalaya: geological aspectsContributed articles. |
From inside the book
Results 1-3 of 79
Page 106
Penninic Nappes and to correlate the Garhwal Nappe instead with the latter
simply because the Garhwal is constituted mainly of metamorphics. Nevertheless
, the absence of metamorphism does not weaken the Indus-Penninic nappe-
analogy ...
Penninic Nappes and to correlate the Garhwal Nappe instead with the latter
simply because the Garhwal is constituted mainly of metamorphics. Nevertheless
, the absence of metamorphism does not weaken the Indus-Penninic nappe-
analogy ...
Page 208
The 7° to l0°N palaeoposition of the Ladakh lntrusives at about 50 m.y. ago, is
rather similar to the contemporaneous palaeolatitude of the part situated south of
the present Indus-Tsangpo suture zone in Ladakh, indicated by palaeomagnetic
...
The 7° to l0°N palaeoposition of the Ladakh lntrusives at about 50 m.y. ago, is
rather similar to the contemporaneous palaeolatitude of the part situated south of
the present Indus-Tsangpo suture zone in Ladakh, indicated by palaeomagnetic
...
Page 297
The granitoids range in age from 235 d: 13 m.y. (Trivedi et al., 198 1 ) to 80 m.y.
and 60 :1: 10 m.y. also 40 m.y. The Ladakh Granitoid Complex borders the entire
Indus Tectonic Zone along its northem margin forming the basement for the ...
The granitoids range in age from 235 d: 13 m.y. (Trivedi et al., 198 1 ) to 80 m.y.
and 60 :1: 10 m.y. also 40 m.y. The Ladakh Granitoid Complex borders the entire
Indus Tectonic Zone along its northem margin forming the basement for the ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Tectonics and Structure of the Pamirs | 9 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 19 |
Peninsular and Himalayan Precambrian Belts | 31 |
Copyright | |
12 other sections not shown
Other editions - View all
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 |
| Export Citation | BiBTeX EndNote RefMan |