Skip to main content
Log in

Shear wave velocity structure beneath the eastern Indian Ocean from Rayleigh wave dispersion measurements

  • Research Article - Solid Earth Sciences
  • Published:
Acta Geophysica Aims and scope Submit manuscript

Abstract

The Eastern Indian Ocean is a tectonically and geodynamically active region that has experienced deformations due to rifting, uplifting, and plume activity. The earlier Rayleigh wave studies in the East Indian Ocean were mainly focused on the structure of the Bay of Bengal, Ninety East Ridge, and Broken Ridge. The structure of other region of the East Indian Ocean is not much explored. In the present study, Rayleigh wave dispersion analysis is performed to observe the signatures of upper mantle deformation in terms of shear wave velocity of the East Indian Ocean using global search method. The fundamental mode Rayleigh wave group velocities are estimated between 15 and 100 s using the multiple filter technique. The group velocities of the raypaths that traverse the same region are clustered (E1–E8) to get an average dispersion curve. Using a genetic algorithm, each cluster's group velocities are inverted for shear velocity structure. The observed dispersion curve of E6, E7, and E8 indicates the lower group velocities between 35 and 100 s relative to E1, E2, E3, E4, and E5, with an average variation of about 0.07–0.18 km/s. The crustal thickness obtained in the study region is ~ 26 km and is due to the increased thickness of the lower crust (9.1–12.4 km) having Vs 3.95–4.04 km/s. The theoretical Vs have been calculated for serpentinite rock at uppermost lithospheric conditions and found to be similar to the Vs of the lower crust in the present study. Hence, it is assumed that unusual crustal thickness is due to the progressive development of the upper lithosphere formation (Ultramafic rock) into material (serpentinite rock) with crustal-like shear velocity or moderately lower than sub-Moho shears velocity. The undeformed lithosphere is evidenced by the high-velocity (Vs 4.62–4.77 km/s) layer beneath the Moho, whose thickness ranges from 41.3 to 51.6 km. The high-velocity lithosphere is followed by a low-velocity zone that extends up to 160 km; however, the variation in Vs (4.57–4.31 km/s) indicates that the low-velocity zone is deformed.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

Code availability (software application or custom code)

No specific code was developed for this work. We have cited the literature on the algorithm.

References

Download references

Acknowledgements

The first author expresses his sincere thanks to Dr. Sumer Chopra (DG), Institute of Seismological Research, for allowing him to carry out part of the research at his facility. The first author expresses his sincere thanks to Prof. M. Ravi Kumar, Prof. R. Hermann, Prof. S.N. Bhattacharya and Dr. K.N.D. Prasad for their valuable suggestions and help. The first author gratefully acknowledges the financial assistance from the University Grants Commission through the Moulna Azad National Fellowship, New Delhi.

Funding

No funding availed for this work.

Author information

Authors and Affiliations

Authors

Contributions

The first author processed the data, determined the Rayleigh wave group velocity, inverted the data for shear velocity structure, wrote the initial draft of the manuscript and finalized the final manuscript. The second author provided the inversion code, assisted the first author in data inversion, provided guidance to the first author, edited the manuscript and finalized the final manuscript. The third author was involved in providing guidance to the first author and involved in the manuscript draft preparation and finalization. Fourth author involved in the manuscript draft preparation. This work has been done as a part of the Ph.D. of the first author, Haseeb Rehman.

Corresponding author

Correspondence to Haseeb Rehman.

Ethics declarations

Conflict of interest

Authors declare that they have no conflicts of interest/competing interest.

Ethics approval

It is declared that we have followed the ethics and integrity in carrying out this work. We approve here to bound by the COPE guidelines.

Consent to participate (include appropriate statements)

We declare our consent to participate in the review process abide by the guidelines of COPE.

Consent for publication

We declare our consent for publication within the guidelines of COPE.

Additional information

Edited by Dr. Rafał Czarny (ASSOCIATE EDITOR) / Prof. Gabriela Fernández Viejo (CO-EDITOR-IN-CHIEF).

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Rehman, H., Sharma, J., Subrahmanyam, M. et al. Shear wave velocity structure beneath the eastern Indian Ocean from Rayleigh wave dispersion measurements. Acta Geophys. 71, 1187–1201 (2023). https://doi.org/10.1007/s11600-023-01045-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11600-023-01045-0

Keywords

Navigation