Himalaya: Geological Aspects, Volume 1P. S. Saklani Contributed articles. |
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Page 11
... formed within the allochthon . Recumbent and overturned folds in the western part of the Central Pamir appeared due to an additional gravitational effect . Essentially , they were formed in such places where a large uplift existed ...
... formed within the allochthon . Recumbent and overturned folds in the western part of the Central Pamir appeared due to an additional gravitational effect . Essentially , they were formed in such places where a large uplift existed ...
Page 177
... formed ( Fig . 12A ) . Axial plane cleavage of the F2 folds formed the S2 cleavage . Some of the normal faults were also developed at this stage of deformation . The origin of the F2 folds obviously depend on the distribution ...
... formed ( Fig . 12A ) . Axial plane cleavage of the F2 folds formed the S2 cleavage . Some of the normal faults were also developed at this stage of deformation . The origin of the F2 folds obviously depend on the distribution ...
Page 321
... formed at greater depths as compared to Kumaun basics . Tangze volcanics indicate their formation at shallower depths and among the Marling , Thidsi and Yugar Nala basics , Thidsi Nala basics indicate higher depths of fractionation as ...
... formed at greater depths as compared to Kumaun basics . Tangze volcanics indicate their formation at shallower depths and among the Marling , Thidsi and Yugar Nala basics , Thidsi Nala basics indicate higher depths of fractionation as ...
Contents
Tectonics and Structure of the Pamirs | 1 |
Metamorphic events in Ladakh Indus suture zone Karakorum | 17 |
Peninsular and Himalayan Precambrian Belts | 31 |
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