Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 65
... phase ( Matum Das tonalite ) is metamorphosed along with its host rock during Late Cretaceous while the younger phase exposed near Gilgit ( 54 ± 4 Ma ) and Shirot ( 40 ± 6 Ma ) is undeformed and associated with Late stage ( 34 + 14 , 29 ...
... phase ( Matum Das tonalite ) is metamorphosed along with its host rock during Late Cretaceous while the younger phase exposed near Gilgit ( 54 ± 4 Ma ) and Shirot ( 40 ± 6 Ma ) is undeformed and associated with Late stage ( 34 + 14 , 29 ...
Page 146
... phase of upheaval was the most violent phase and it took place in the Middle Miocene . During this very phase almost the present configuration of the Himalaya was carved out . This phase culminated in severe folding , overturning and ...
... phase of upheaval was the most violent phase and it took place in the Middle Miocene . During this very phase almost the present configuration of the Himalaya was carved out . This phase culminated in severe folding , overturning and ...
Page 162
... phases of deformation are present ( Naha and Ray , 1971 ) . It has been observed that away from the thrusts all the three phases of deformation are dominant but at or near the thrust faults the third phase of folding is more prominent ...
... phases of deformation are present ( Naha and Ray , 1971 ) . It has been observed that away from the thrusts all the three phases of deformation are dominant but at or near the thrust faults the third phase of folding is more prominent ...
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