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. |
From inside the book
Results 1-3 of 30
Page 18
... collision between the Indo - Himalayan and the Tibetan continents ( Fig . 3E ) . The Shilakong ( Spong and Photang ) ... zone and thus the extent of later post - colli- sional indentation of the Indian continent into the Himalayan and Tibetan ...
... collision between the Indo - Himalayan and the Tibetan continents ( Fig . 3E ) . The Shilakong ( Spong and Photang ) ... zone and thus the extent of later post - colli- sional indentation of the Indian continent into the Himalayan and Tibetan ...
Page 107
... collision zone and ( ii ) Central Crystalline zone of the High Himalaya . The magmatic growth in the western part of the Indus - Yarlung collision zone started with the initiation of the Dras island arc in the Ladakh and Kohistan ...
... collision zone and ( ii ) Central Crystalline zone of the High Himalaya . The magmatic growth in the western part of the Indus - Yarlung collision zone started with the initiation of the Dras island arc in the Ladakh and Kohistan ...
Page 114
... zone ( characterised by a distinct assemblage of mafic and ultramafic rocks , deep marine sediments with radiolarites and andesitic rocks ) represents the collision zone between the Indian and the Eurasian plates ( Dewey and Bird , 1970 ...
... zone ( characterised by a distinct assemblage of mafic and ultramafic rocks , deep marine sediments with radiolarites and andesitic rocks ) represents the collision zone between the Indian and the Eurasian plates ( Dewey and Bird , 1970 ...
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 | |
5 other sections not shown
Other editions - View all
Common terms and phrases
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