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Variability of orographic architecture of Indo-Burmese Ranges (NE India) : constraints from morphotectonic and lineament analysis

Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Activeness of the tectonic and related sub-surface processes control the surface features that lead to variations in topography and lithostratigraphy. To understand the role of active tectonis in shaping the topography, morphotectonic and lineament studies are important. In this study, geological categorization has helped understand the orogenic evolution of the Indo-Burmese Range (IBR), NE India. This is an arcuate hill range that shows many unique topographic characteristics that incited to categorise the entire IBR into different tectonically active domains: Northern (Changlang district of Arunachal Pradesh); Naga Hills; Cachar and Manipur; and Southern (Mizoram). The Northern and Southern domains are more active than the others. Lineament analysis also indicates the presence of active features in the region with NW-SE, NE-SW, ESE-WNW trends are being common. The Northern and Naga Hills domains have mostly E-W younger lineaments whereas the Cachar and Manipur domains rather show N-S younger trends. The Southern Mizoram domain shows a dominance of older N-S lineaments with younger NW-SE lineaments. These variations result from differential stress conditions, i.e. Indian Plate movement and westward stress from the Burma Plate. This study shows how overall variations in tectonic settings can be related to the orogenic evolution.
Rocznik
Strony
130--140
Opis fizyczny
Bibliogr. 33 poz., fot., rys., tab.
Twórcy
  • Dibrugarh University, Department of Applied Geology, Dibrugarh - 786004, Assam, India
  • Dibrugarh University, Department of Applied Geology, Dibrugarh - 786004, Assam, India
autor
  • Dibrugarh University, Department of Applied Geology, Dibrugarh - 786004, Assam, India
  • Pachhunga University College, Department of Geology, Aizawl - 796007, Mizoram, India
Bibliografia
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  • 4. Cox, R.T., 1994. Analysis of drainage basin symmetry as a rapid technique to identify areas of possible Quaternary tilt-block tectonics: an example from the Mississippi Embayment. GSA Bulletin, 106: 571-581.
  • 5. Hack, J.T., 1973. Stream-profile analysis and stream-gradient index. Journal of Research of the U.S. Geological Survey, 1: 421-429.
  • 6. Hare, P.W., Gardner, T.W., 1985. Geomorphic indicators of vertical neotectonism along converning plate margins, Nicoya Peninsula, Costa Rica In: Tectonic Geomorphology (eds. M. Morisawa and J.T. Hack): 75-104. Proceedings of the 15th Annual Bighampton Geomorphology Symposium.
  • 7. Howard, A.D., 1967. Drainage analysis in geologic interpretation: a summation. AAPG Bulletin, 51: 2246-2259.
  • 8. Kania, M., 2015. Microstructures of shear zones from selected domains of the Western Tatra Mountains. Geological Quarterly, 59 (4): 679-699.
  • 9. Keller, E.A., Pinter, N., 2002. Active Tectonics: Earthquakes, Uplift, and Landscape. New Jersey, Prentice Hall.
  • 10. Kowalski, A., 2017. Fault geometry and evidence of depocentre migration within a transtensional intra-basinal high - a case study from the Łączna Anticline (Intrasudetic Synclinorium, SW Poland). Geological Quarterly, 61 (4): 779-794.
  • 11. Krzywiec, P., Gutowski, J., Walaszczyk, I., Wróbel, G., Wybraniec, S., 2009. Tectonostratigraphic model of the Late Cretaceous inversion along the Nowe Miasto-Zawichost Fault Zone, SE Mid-Polish Trough. Geological Quarterly, 53 (1): 27-48.
  • 12. Masoud, A., Koike, K., 2006. Tectonic architecture through Landsat-7 ETM+/SRTM DEM-derived lineaments and relationship to the hydrogeologic setting in Siwa region, NW Egypt. Journal of African Earth Sciences, 45: 467-477.
  • 13. Masoud, A.A., Koike, K., 2011. Morphotectonics inferred from the analysis of topographic lineaments auto-detected from DEMs: application and validation for the Sinai Peninsula, Egypt. Tectonophysics, 510: 291-308.
  • 14. O’Leary, D.W., Friedman, J.D., Pohn, H.A., 1976. Lineament, lineation. Some proposed new standards for old terms. GSA Bulletin, 87: 1463-1469.
  • 15. Pirasteh, S., Pradhan, B., Safari, H.O., Ramli, M.F., 2013. Coupling of DEM and remote-sensing-based approaches for semi-automated detection of regional geostructural features in Zagros mountain, Iran. Arabian Journal of Geosciences, 6: 91-99.
  • 16. Ramírez-Herrera, M.T., 1998. Geomorphic assessment of active tectonics in the Acambay Graben, Mexican volcanic belt. Earth Surface Processes and Landforms, 23: 317-332.
  • 17. Rakshit, R., Bezbaruah, D., 2016. Morphotectonic aspects in and around Aizawl, Mizoram of NE India. South East Asian Journal of Sedimentary Basin Research, 2-3: 28-36.
  • 18. Rakshit, R., Lalhmingsangi, D., Bezbaruah, D., Bharali, B., 2017. Morphotectonic and sedimentological aspects in describing the relationship with ancient failure surfaces in southern part of Aizawl anticline, Mizoram, India. Science Vision, 17: 204-216.
  • 19. Rakshit, R., Bezbaruah, D., Bharali, B., 2018. Oblique slip faulting associated with evolving central Indo-Burmese region from Early Pleistocene deformational sequences. Solid Earth Sciences, 3: 67-80.
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  • 21. Seleem, T.A., 2013. Analysis and tectonic implication of DEM-derived structural lineaments, Sinai Peninsula, Egypt. International Journal of Geosciences, 4: 183-201.
  • 22. Singh, A.K., Chung, S.L., Bikramaditya, R.K., Lee, H.Y., 2017. New U-Pb zircon ages of plagiogranites from the Nagaland-Manipur Ophiolites, Indo-Myanmar Orogenic Belt, NE India. Journal of the Geological Society, 174: 170-179.
  • 23. Solomon, S., Ghebreab, W., 2006. Lineament characterization and their tectonic significance using Landsat TM data and field studies in the central highlands of Eritrea. Journal of African Earth Sciences, 46: 371-378.
  • 24. Steckler, M.S., Mondal, D.R., Akhter, S.H., Seeber, L., Feng, L., Gale, J., Hill, E.M., Howe, M., 2016. Locked and loading megathrust linked to active subduction beneath the Indo-Burman Ranges. Nature Geoscience, 9: 615-618.
  • 25. Šimonova, V., Plašienka, D., 2017. Stepwise clockwise rotation of the Cenozoic stress field in the Western Carpathians as revealed by kinematic analysis of minor faults in the Manín Unit (western Slovakia). Geological Quarterly, 61 (1): 251-264.
  • 26. Šliaupa, S., Satkūnas, J., Motuza, G., Šliaupienė, R., 2017. Morphotectonic implication of the Paleoproterozoic Mid-Lithuanian Suture Zone. Geological Quarterly, 61 (3): 590-601.
  • 27. Twidale, C.R., 2004. River patterns and their meaning. Earth-Science Reviews, 67: 159-218.
  • 28. Urbano, T., Piacentini, T., Buccolini, M., 2017. Morphotectonics of the Pescara River basin (Central Italy). Journal of Maps, 13: 511-520.
  • 29. Wang, Y., Sieh, K., Tun, S.T., Lai, K.-Y., Myint, T., 2014. Active tectonics and earthquake potential of the Myanmar region. Journal of Geophysical Research: Solid Earth, 119: 3767-3822.
  • 30. Webb, A.A.G., Guo, H., Clift, P.D., Husson, L., Muller, T., Costantino, D., Yin, A., Xu, Z., Cao, H., Wang, Q., 2017. The Himalaya in 3D: slab dynamics-controlled mountain building and monsoon intensification. Lithosphere, 9: 637-651.
  • 31. Yajuan, H., Fei, W., Quan, W., Qingfa, W., 2008. Change patterns of linear features in remote sensing images in land use. Transactions of the Chinese Society of Agricultural Engineering, 2008: 12.
  • 32. Zaman, F., Bezbaruah, D., 2019. Morphotectonic aspects in a part of Naga-Schuppen belt, Assam Nagaland region, Northeast India. Science Vision, 19. 6-11.
  • 33. Zaman, F., Bezbaruah, D., Lalhmingsangi, D., Rakshit, R., 2019. Morphotectonic study in a part of Indo-Burmese Ranges in Eastern Mizoram, India. Senhri Journal of Multidisciplinary Studies, 3: 81-92.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e737d7e5-74af-4fcd-ba6e-28a099cd571a
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