Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 89
... Fault as well as the Himalayan Front Fault ( Nakata , 1972 , 1975 ) . The frontal zone is tectonically most active in the Himalaya at present and an average vertical slip rate along the zone is altogether calculated as 3-4 mm per year ...
... Fault as well as the Himalayan Front Fault ( Nakata , 1972 , 1975 ) . The frontal zone is tectonically most active in the Himalaya at present and an average vertical slip rate along the zone is altogether calculated as 3-4 mm per year ...
Page 91
... Fault appears roughly along the geological Kali Gandaki - Bari Gad fault . This active fault extends approximately in the NW - SE direction for 140 km . The fault is recognized ... Fault The Himalayan Active Faults : Tectonic Significance 91.
... Fault appears roughly along the geological Kali Gandaki - Bari Gad fault . This active fault extends approximately in the NW - SE direction for 140 km . The fault is recognized ... Fault The Himalayan Active Faults : Tectonic Significance 91.
Page 170
... fault surface . Deformation of a series of basement faults with varying amounts of dip and curvature produced fault displacement along some of the faults whereas the other faults remained inactive . 6. Fault displacement was accompanied ...
... fault surface . Deformation of a series of basement faults with varying amounts of dip and curvature produced fault displacement along some of the faults whereas the other faults remained inactive . 6. Fault displacement was accompanied ...
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