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Titlebook: Structural Geometry of Mobile Belts of the Indian Subcontinent; Tapas Kumar Biswal,Sumit Kumar  Ray,Bernhard Grase Book 2020 Springer Natu

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Tectonic Development of the Bengal Basin in Relation to Fold-Thrust Belt to the East and to the Nor, and Stable Indian Craton to the west. To the north, convergence tectonic loading presumed to transfer from the deformation front, along the Oldham and Dauki faults to the south and shaped not only the Shillong Plateau and Assam Basin, but also the northern part of the Bengal Basin. To the east, ob
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Structural Imprints of Andaman Accretionary Prism and Its Tectonic Relation with Ophiolite Belt of f Upper Cretaceous ophiolite and Eocene sediments is exposed in Andaman Islands. Map pattern and the field distribution show dismembered ophiolites occurring in different N-S trending thrust slices where the western slices have low dip (8°–10°) and the eastern slices have steep dip (65°–70°) towards
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Anisotropy of Magnetic Susceptibility (AMS) Studies on Quartzites of Champaner Group, Upper Aravallantly present within each formation of the Champaner Group, they have been selected for the study. Our study on AMS signifies two prominent striking planes of magnetic foliation within the rocks. The rocks have (i) ENE-WSW to E-W and (ii) N-S to NE-SW trends. The former trend matches with the region
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Thrust Sheets, Tectonic Windows, and Intermontane Basins in the Nepal Himalaya,tal issues of their stratigraphy and structure are still unresolved. Especially, there has been considerable controversy over delineating the Greater Himalayan and Lesser Himalayan belts of Nepal. The Greater Himalayan thrust sheet represents the hanging wall of the Main Central Thrust. In Nepal, th
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Book 2020mpling and analysis work (e.g. petrographic studies), as well as limited geochemical and geochronological analysis to support the findings. A discussion on the structural evolution of these mobile belts and their connections with other belts rounds out the coverage..
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