Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 56
... region from the rest of the area . This region , marked by positive anomalies , reflect undercompensated masses . Such a configuration could be explained in terms of either upwarping of mantle or a large scale lateral heterogeneity ...
... region from the rest of the area . This region , marked by positive anomalies , reflect undercompensated masses . Such a configuration could be explained in terms of either upwarping of mantle or a large scale lateral heterogeneity ...
Page 259
... region ( 32.5 ° -33.5 ° N , 75.5 ° -76.5 ° E ) and the Kinnaur region ( 31.5-33.0 ° N , 78-79 ° E ) are characterized by appreciable seismicity . As explained by Ni and Barazang ( 1984 ) , Verma and Kumar ( 1987 ) , Chatterjee and ...
... region ( 32.5 ° -33.5 ° N , 75.5 ° -76.5 ° E ) and the Kinnaur region ( 31.5-33.0 ° N , 78-79 ° E ) are characterized by appreciable seismicity . As explained by Ni and Barazang ( 1984 ) , Verma and Kumar ( 1987 ) , Chatterjee and ...
Page 262
... Region This region mostly includes the Nepalese Himalaya extending from 80 ° to 88 ° E , 26.5 ° to 31 ° N . This is one of the most active regions of the Himalaya . Seismicity in this region has been discussed in detail by Pandey et al ...
... Region This region mostly includes the Nepalese Himalaya extending from 80 ° to 88 ° E , 26.5 ° to 31 ° N . This is one of the most active regions of the Himalaya . Seismicity in this region has been discussed in detail by Pandey et al ...
Contents
Tectonics and Structure of the Pamirs | 1 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 17 |
Peninsular and Himalayan Precambrian Belts | 31 |
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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