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Shear-wave velocity models in and around north-east India by modelling Rayleigh wave group velocity dispersion data

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Abstract

Rayleigh wave group velocity dispersion data of moderate magnitude (Mw 5.4) earthquake of Assam, North-East (NE) India, is used to retrieve regional shear wave crustal velocity models. The earthquake located within the northeast part of the Indian continent is well recorded by 10 broadband seismic stations situated on the Indian, Eurasian, and Burmese plates to generate excellent Rayleigh waveforms. Wave propagation paths transverse different geotectonic units in the collision zones of India–Eurasia and India–Burmese in and around NE India. We divide the data into outer and inner station groups depending on epicentre distance. Paths of the inner group mainly pass through the Indian plate, and the outer group crosses the inter-continent zones. The dispersion data and corresponding shear wave structure are not dependent on group division or epicentre distance, indicating diversity in the tectonic and geological setup. Paths crossing the Bengal basin (BB) with thick sediment layers have low velocities, and older crystalline rocks of the Shillong Plateau and Himalayan region have high velocities in the uppermost 10–15 km crust. A very high contrast of crustal velocity is noticed along the paths of Agartala (AGART) and Dhubri (DHUB) stations located at similar epicentre distances and an azimuthal difference of only 55°. Path to AGART along the BB has very low crustal velocities, while DHUB along the entire Shillong Plateau region has very high velocities. Four stations of the inner group within the Indian plate have a high difference in crustal velocities: low velocities within thick sediments of BB and high velocities in the older crystalline rocks of the Shillong plateau. In contrast, in the northern part of the Indo-Burma subduction zone, the subsurface structure shows repeated underthrusting of low-velocity material from the down-going plate and over-thrusting of high-velocity material from the overriding plate.

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Acknowledgements

We are very grateful to the India Meteorological Department (IMD) and IRIS website for providing earthquake waveform data for this study. The first author would like to thank all authors and supervisors for supporting this work and the Ministry of Human Resource Development (MHRD) for providing a fellowship. We are all very grateful to the two unknown reviewers whose comments and suggestions helped us significantly improve the manuscript.

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Nongmaithem Menaka Chanu: Methodology, validation, formal analysis, data curation, and writing the original draft. Naresh Kumar: Conceptualisation, validation, investigation, resources, writing – review & editing, supervision. Vivek G Babu: Validation, formal analysis and data curation. Sagarika Mukhopadhyay: Conceptualization, validation, investigation, resources, writing – review & editing, supervision, and funding acquisition. Amit Kumar: Validation, formal analysis and data curation.

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Correspondence to Naresh Kumar.

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Communicated by Arkoprovo Biswas

Supplementary materials pertaining to this article are available on the Journal of Earth System Science website (http://www.ias.ac.in/Journals/Journal_of_Earth_System_Science).

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Chanu, N.M., Kumar, N., Babu, V.G. et al. Shear-wave velocity models in and around north-east India by modelling Rayleigh wave group velocity dispersion data. J Earth Syst Sci 132, 170 (2023). https://doi.org/10.1007/s12040-023-02193-z

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