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 9
... Tethyan Himalaya to the north . The orogen possibly evolved through a two stage process : a ) fragmentation of the Pan - Indian continent mainly during late Mesozoic and creation of narrow peri - Indian oceans which were flanked by ...
... Tethyan Himalaya to the north . The orogen possibly evolved through a two stage process : a ) fragmentation of the Pan - Indian continent mainly during late Mesozoic and creation of narrow peri - Indian oceans which were flanked by ...
Page 10
... Tethyan Him- alaya to the north . The Phanerozoic epicontinental sediments have Tethyan faunal , as well as , Gondwanic facies and floral - faunal intercalations . The Lesser Himalayan belt with mainly Pro- terozoic and truncated ...
... Tethyan Him- alaya to the north . The Phanerozoic epicontinental sediments have Tethyan faunal , as well as , Gondwanic facies and floral - faunal intercalations . The Lesser Himalayan belt with mainly Pro- terozoic and truncated ...
Page 19
... Tethyan Himalaya had arrived almost as far north as it is today . Convergence of Indian plate since this period is taken up mainly along the MCT and its splays . A complex im- bricated crustal and subcrustal structure for the Himalaya ...
... Tethyan Himalaya had arrived almost as far north as it is today . Convergence of Indian plate since this period is taken up mainly along the MCT and its splays . A complex im- bricated crustal and subcrustal structure for the Himalaya ...
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