Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 111
... Main Central Thrust , became no longer open as a passage down to the mantle level . It was replaced in turn by the more external Main Boundary Fault since Pliocene time . The Main Boundary Fault provided a new crustal inlet for the ...
... Main Central Thrust , became no longer open as a passage down to the mantle level . It was replaced in turn by the more external Main Boundary Fault since Pliocene time . The Main Boundary Fault provided a new crustal inlet for the ...
Page 338
... Main Boundary Fault . In Kashmir no thrust equivalent in magnitude or extension to the Main Central Thrust exists . The Main Boundary Fault itself is split into two major faults viz . the so called Main Boundary Fault ( Middlemiss ...
... Main Boundary Fault . In Kashmir no thrust equivalent in magnitude or extension to the Main Central Thrust exists . The Main Boundary Fault itself is split into two major faults viz . the so called Main Boundary Fault ( Middlemiss ...
Page 411
... Main Boundary Thrust and further to the north , the Tibetan Series are bounded by Main Central Thrust . The Nepalese Series occurs in the form of a huge antiform mainly constituted by quartzopelitic rocks lying along the axial extension ...
... Main Boundary Thrust and further to the north , the Tibetan Series are bounded by Main Central Thrust . The Nepalese Series occurs in the form of a huge antiform mainly constituted by quartzopelitic rocks lying along the axial extension ...
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