Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 417
... Tibetan plateau ( 5000 to 6000m ) , the tectonics becomes less complicated . Structural discontinuities exist at the passage between the folded Tibetan series and the Tibetan slab . At its basal part , the Tibetan slab overlies a series ...
... Tibetan plateau ( 5000 to 6000m ) , the tectonics becomes less complicated . Structural discontinuities exist at the passage between the folded Tibetan series and the Tibetan slab . At its basal part , the Tibetan slab overlies a series ...
Page 425
... Tibetan slab It is sure that the Tibetan slab extends not only in Nepal , but beyond the India - Nepal border also . ( a ) Western Nepal : The Tibetan series are well developed at Tsum land and between Kali Gandaki and Thulo Bheri , but ...
... Tibetan slab It is sure that the Tibetan slab extends not only in Nepal , but beyond the India - Nepal border also . ( a ) Western Nepal : The Tibetan series are well developed at Tsum land and between Kali Gandaki and Thulo Bheri , but ...
Page 426
... Tibetan zone . Similar is the case of the Kashmir Himalaya . THE GEOLOGICAL INTERPRETATION OF TIBETAN SLAB The age of Tibetan slab The oldest sedimentary formations of the folded Tibetan series based on fossil records have been dated as ...
... Tibetan zone . Similar is the case of the Kashmir Himalaya . THE GEOLOGICAL INTERPRETATION OF TIBETAN SLAB The age of Tibetan slab The oldest sedimentary formations of the folded Tibetan series based on fossil records have been dated as ...
Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
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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