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Mantle deformation and seismic anisotropy beneath Northeast India inferred from SKKS birefringence

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Abstract

The present study produces very new SKKS splitting measurements from the Northeast India, suggesting the region as tectonically more heterogeneous and complex in nature. It fills the gap of anisotropic parameters from an epicentral range of 140°–180° in order to understand the lithospheric deformation patterns of the terrain in a better way. The splitting parameters namely polarisation direction of fast waves (ϕ) and delay time are the manifestation of anisotropic effects of a medium. The present SKKS splitting measurements from nine broadband seismic stations in Northeast India incorporate new understandings of deformation patterns for this region. At the Himalayan collision zone and sub-Himalayan region, the deformation pattern showing a perfect alignment of the ϕ parallel to the collisional arc (Main Boundary Thrust, Main Central Thrust), suggests that a localized strain derived from N-S Indo-Eurasian collision is the major source behind its complex tectonics. The SKKS splitting measurements at Assam foredeep region streamline the effect of Kopili fault in controlling the deformation patterns in a NW-SE direction. There is a significant difference in anisotropic behaviour of stations at the northern Shillong plateau compared to the stations at its southern proximity. The absolute plate motion (APM) parallel to ϕ in northern fringe of the plateau strictly indicates the influence of asthenospheric flow, which in turn is driven by APM of Indian plate in a no net rotation reference frame. On the other hand, major regional structures like the Dauki and Dapsi faults control the anisotropic pattern at the southern extremity of this plateau.

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Acknowledgements

DDM acknowledges the permission and support provided by Director, CSIR-NEIST, for utilization of data in research work and its publication (NMN-202022). The authors are also thankful to National Geophysical Research Institute (NGRI), Hyderabad and Ministry of Earth Sciences (MoES) for providing seismological data. The study is supported by Early Career Research Grant from Science and Engineering Research Board (SERB), India (Grant No. ECR/2018/001293). PM acknowledges the Department of Science and Technology (DST) for fellowship grant (Inspire Fellowship No. IF180255) and Academy of Scientific and Innovative Research (AcSIR) for academic support.

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Correspondence to Debasis D. Mohanty.

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Mondal, P., Mohanty, D.D. Mantle deformation and seismic anisotropy beneath Northeast India inferred from SKKS birefringence. Stud Geophys Geod 65, 36–52 (2021). https://doi.org/10.1007/s11200-020-1121-y

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  • DOI: https://doi.org/10.1007/s11200-020-1121-y

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