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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... Main Central Thrust is represented by the boundary between the low grade and medium grade metamorphics while the Upper Main Central Thrust is characterized by the high grade gneisses , migmatites and orthogneisses . Recent researches ...
... Main Central Thrust is represented by the boundary between the low grade and medium grade metamorphics while the Upper Main Central Thrust is characterized by the high grade gneisses , migmatites and orthogneisses . Recent researches ...
Page 39
... Main Central Thrust . During the formation of the relief thrusts the zone of the Main Central Thrust was reactivated alongwith intense rock deformation . INTRODUCTION Geological research started in the Himalayas 130 years ago . The ...
... Main Central Thrust . During the formation of the relief thrusts the zone of the Main Central Thrust was reactivated alongwith intense rock deformation . INTRODUCTION Geological research started in the Himalayas 130 years ago . The ...
Page 91
... Main Central Thrust and occur as inliers of Baijnath and Askot and beyond Main Central Thrust , or Central Crystalline Zone , the root zone . Coarsely crystalline and metamor- phosed up to Garnet - Staurolite grade , the rocks contain ...
... Main Central Thrust and occur as inliers of Baijnath and Askot and beyond Main Central Thrust , or Central Crystalline Zone , the root zone . Coarsely crystalline and metamor- phosed up to Garnet - Staurolite grade , the rocks contain ...
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