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 13
... Paleozoic Tectonism and Magmatism Late Paleozoic sediments in the Himalaya , consisting of basal Gondwana diamictites with fluxoturbiditic greywackes and other sediments are closely associated with contemporaneous volcanics ( Acharyya ...
... Paleozoic Tectonism and Magmatism Late Paleozoic sediments in the Himalaya , consisting of basal Gondwana diamictites with fluxoturbiditic greywackes and other sediments are closely associated with contemporaneous volcanics ( Acharyya ...
Page 18
... Paleozoic sediments occurring at the lowest tectonic levels is inferred to be close to the MBT zone . Similarly in the Siang valley window , the Abor volcanics with Late Paleozoic and Cretaceous - Eocene components occur close to the ...
... Paleozoic sediments occurring at the lowest tectonic levels is inferred to be close to the MBT zone . Similarly in the Siang valley window , the Abor volcanics with Late Paleozoic and Cretaceous - Eocene components occur close to the ...
Page 20
... Paleozoic failed rifts affected various parts of the Pan - Indian continent , especially the northern and the southern margins of the Himalayan microcontinent and parts of Tibet , and narrow Permian oceans might have been created ...
... Paleozoic failed rifts affected various parts of the Pan - Indian continent , especially the northern and the southern margins of the Himalayan microcontinent and parts of Tibet , and narrow Permian oceans might have been created ...
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