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 59
... trend . In the quartzite specimens selected for strain analysis , the main foliation repre- sents the xy plane of ... trends parallel to the thrust transport direction . This can be explained by the fact that the NW - SE stretching was ...
... trend . In the quartzite specimens selected for strain analysis , the main foliation repre- sents the xy plane of ... trends parallel to the thrust transport direction . This can be explained by the fact that the NW - SE stretching was ...
Page 90
... trend ( Table 4 ) . So it can be inferred that the quarter wavelength / amplitude ratio was directly proportional to ... TRENDS IN GEOLOGY – XI HIMALAYAN MOUNTAIN BUILDING : 90.
... trend ( Table 4 ) . So it can be inferred that the quarter wavelength / amplitude ratio was directly proportional to ... TRENDS IN GEOLOGY – XI HIMALAYAN MOUNTAIN BUILDING : 90.
Page 157
... trend . This folding is very dominant in the western part of the area . In the eastern part trend lines are not seen over long distance due to massive or soft nature of rock cover and hence delineation of precise nature of folding is ...
... trend . This folding is very dominant in the western part of the area . In the eastern part trend lines are not seen over long distance due to massive or soft nature of rock cover and hence delineation of precise nature of folding is ...
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