Himalayan Mountain BuildingThe Mchanisms Expounded By Suess, Followed By The Classical Gwosynclinal Concept Of Mountain Building And The Theory Of Continental Drift Etc., Have Been Assimilated In The Plate Tectonic Concepts And Their Applications Towards Understanding The Integrated Evolutionary History Of The Global Features In The Mesozoic-Cenozoic Time-Space Domain. |
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Page 24
... Lhasa - Xigaze region , Tibet . Earth Planet Sci . Lett . , 69 : 311-320 . Scharer , U. , Xu , R.H. and Allegre , CJ . 1986. U- ( Th ) -Pb systematics and ages of Himalayan leucogranites , South Tibet . Earth Planet . Sci . Lett . , 77 ...
... Lhasa - Xigaze region , Tibet . Earth Planet Sci . Lett . , 69 : 311-320 . Scharer , U. , Xu , R.H. and Allegre , CJ . 1986. U- ( Th ) -Pb systematics and ages of Himalayan leucogranites , South Tibet . Earth Planet . Sci . Lett . , 77 ...
Page 134
... Lhasa block . Han Tonglin and Wang Naiwen ( 1983 ) , accordingly , conclude that the glacial deposits suggest that " Quinghai - Xizang , as well as the Indian shield was ( were ) united as a palaeocontinent and is ( were ) indivisible ...
... Lhasa block . Han Tonglin and Wang Naiwen ( 1983 ) , accordingly , conclude that the glacial deposits suggest that " Quinghai - Xizang , as well as the Indian shield was ( were ) united as a palaeocontinent and is ( were ) indivisible ...
Page 196
... Lhasa was obtained to be 20 ° N ( during Cretaceous times ) . During this period the Indian land- mass was very much in the southern hemisphere with Nagpur close to 30 ° S latitude ( Verma , 1973 ) . It appears from the tentative ...
... Lhasa was obtained to be 20 ° N ( during Cretaceous times ) . During this period the Indian land- mass was very much in the southern hemisphere with Nagpur close to 30 ° S latitude ( Verma , 1973 ) . It appears from the tentative ...
Contents
Hidden Central Indian Ridge and Himalayan Mountain System | 27 |
Microstructural Strain Path in Pratapnagar Quartzite Yamuna Valley | 45 |
Analysis of Folds in Dharkot Thrust Sheet | 63 |
Copyright | |
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Acharyya Allegre amphibolites batholith calc-alkaline Central Crystalline collision zone compression continent continental crustal Deccan traps deformation Delhi Dras Earth Planet emplacement Eocene evolution F3 folds faults flattening formations Gansser Garhwal Geol Geology Geophys gneisses Gondwana Gondwanaland granite granitoid Himal Himalaya Indian plate Indus Suture Indus-Tsangpo island arc Klootwijk Kohistan Krol Belt Kumaun Kumaun Himalaya Ladakh Late Cretaceous Late Paleozoic Lesser Himalaya leucogranites Lhasa LILY lineament magmatic Main Central Thrust margin Merh Mesozoic metamorphism microcontinent Mizoram movement nappe Nepal northern northward oceanic crust ophiolite orogeny P.S. Saklani Pakistan palaeomagnetic Paleozoic Permian plate tectonic plateau plutons pole positions Precambrian quartz grains quartzite ratio Rb-Sr region ridge rift rocks Scharer schists secondary components sediments sequence Sharma Shyok strain structural studies subduction suture Suture Zone Tectonophysics Tertiary Tethyan Tethys Thakur thrust sheet Tibet Today & Tomorrow's Tomorrow's Printers trend Triassic uplift Valdiya volcanics Yamnotri