Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
From inside the book
Results 1-3 of 8
Page 57
... values . However , the measured heat flow values ( Gupta and Rao , 1970 ; Gupta , 1982 ; Gupta et al . , 1982 ) are normal ranging from 40-70 mW / m . DISCUSSION In view of the striking paralllelism between the central Indian ridge and ...
... values . However , the measured heat flow values ( Gupta and Rao , 1970 ; Gupta , 1982 ; Gupta et al . , 1982 ) are normal ranging from 40-70 mW / m . DISCUSSION In view of the striking paralllelism between the central Indian ridge and ...
Page 215
... values for the Ladakh region are not unexpected as they most probably include several hundred kilometers of convergence taken up by closure of the supposed marginal basin . It must be stressed that the magnitude of this convergence ...
... values for the Ladakh region are not unexpected as they most probably include several hundred kilometers of convergence taken up by closure of the supposed marginal basin . It must be stressed that the magnitude of this convergence ...
Page 218
... values for about 2500 km for the western and more eastern regions of the Hindu Kush - Pamir - Karakorum - Himalayan chain ( Fig . 10 , Table VIII , IX ) . This is a puzzling observation as these data , although based in part on ...
... values for about 2500 km for the western and more eastern regions of the Hindu Kush - Pamir - Karakorum - Himalayan chain ( Fig . 10 , Table VIII , IX ) . This is a puzzling observation as these data , although based in part on ...
Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
8 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 chlorite collision continental Cretaceous crust crustal deformation deposits earthquakes eastern Eocene facies flysch folds foreland formation Gansser Garhwal garnet Geodynamics Geol Geology Geophys geosyncline gneiss Gondwana granite Higher Himalaya Himalaya Indian plate Indian Shield Indus Suture island arc Jour Karakorum Kashmir Klootwijk Krol Kumaun Ladakh Late Lesser Himalaya limestone Lower magmatic Main Boundary Main Central Thrust margin melange Mesozoic metamorphism Molnar movement nappe Nepal northern northward occur oceanic ophiolite orogenic Pakistan Palaeocene palaeomagnetic Palaeozoic Pamir Pande Panjal Permian phase plate tectonics Plateau Precambrian Proterozoic quartzite Quetta Range region rocks rotation Saklani sandstones Saxena schists sedimentary sediments seismicity sequence serpentinite Sharma Shyok Simla Siwalik southern stratigraphic structural Surv suture zone Tectonic Zone Tectonophysics Tertiary Tethyan Tethys thickness Tibet Tibetan slab Triassic Upper Valdiya volcanics