Articles | Volume 17, issue 10
https://doi.org/10.5194/se-17-1201-2026
https://doi.org/10.5194/se-17-1201-2026
Research article
 | 
20 Oct 2026
Research article |  | 20 Oct 2026

Mantle deformation patterns beneath the Central India Tectonic Zone: evidence from SK(K)S splitting measurements in the Satpura Gondwana Basin and adjacent areas

Nitarani Bishoyi, Arun Kumar Dubey, and Ashwani Kant Tiwari

Cited articles

Acharya, S.: Evolutionary characters of the Gondwanic Indian crust, Indian Minerals, 51, 1–24, 1997. a
Acharyya, S.: The nature of Mesoproterozoic Central Indian Tectonic Zone with exhumed and reworked older granulites, Gondwana Res., 6, 197–214, https://doi.org/10.1016/s1342-937x(05)70970-9, 2003. a, b
Altamimi, Z., Métivier, L., Rebischung, P., Collilieux, X., Chanard, K., and Barnéoud, J.: ITRF2020 Plate Motion Model, Geophys. Res. Lett., 50, https://doi.org/10.1029/2023gl106373, 2023. a
Babuska, V. and Cara, M.: Seismic Anisotropy in the Earth, Springer Netherlands, ISBN 9789401136006, https://doi.org/10.1007/978-94-011-3600-6, 1991. a
Barruol, G. and Mainprice, D.: A quantitative evaluation of the contribution of crustal rocks to the shear-wave splitting of teleseismic SKS waves, Phys. Earth Planet. In., 78, 281–300, https://doi.org/10.1016/0031-9201(93)90161-2, 1993. a, b, c, d, e
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Short summary
This study examines shear wave splitting of core-refracted seismic phases from earthquakes to determine seismic anisotropy in unexplored areas of Central India. Understanding seismic anisotropy is essential for gaining insights into past geodynamic processes and current tectonic activities in the area. Our findings show that mantle deformation is influenced by both present plate motion and prior orogenic events, such as subduction, collision, and mantle plume activity within the study region.
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