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 10
... Himalaya , and the Oligo - Miocene back - deep molasse in the ITO zone were affected by schuppen structures . Transverse and oblique faults and lineaments were also produced cutting across the Himalaya ... Lesser Himalaya to the south and the ...
... Himalaya , and the Oligo - Miocene back - deep molasse in the ITO zone were affected by schuppen structures . Transverse and oblique faults and lineaments were also produced cutting across the Himalaya ... Lesser Himalaya to the south and the ...
Page 13
... Lesser Himalaya have a prominent stratigraphic break at their base against the older meta - sediments which are essentially Precambrian in age . In the Tethyan Himalayan belt , however , the infra- Gondwana stratigraphic break though ...
... Lesser Himalaya have a prominent stratigraphic break at their base against the older meta - sediments which are essentially Precambrian in age . In the Tethyan Himalayan belt , however , the infra- Gondwana stratigraphic break though ...
Page 41
... Himalaya comprising the Central Crystalline and the Tibetan Zone - was overriding the Lesser Himalayan units . The crystallines were at that time in the state of active regional metamorphism . It can be demonstrated how the mineral ...
... Himalaya comprising the Central Crystalline and the Tibetan Zone - was overriding the Lesser Himalayan units . The crystallines were at that time in the state of active regional metamorphism . It can be demonstrated how the mineral ...
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