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. 2023 Oct 28;13:18488. doi: 10.1038/s41598-023-42722-w

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© The Author(s) 2023

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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The subsurface resistivity section (TM mode) of the Rohtak region overlapped with the seismicity of magnitude 2.0 ≤ M ≤ 2.9 (shown with black dots) occurred between latitude 28°N–29.5°N and longitude 76°E–77°E from January 2000 to April 2022 taken from https://seismo.gov.in/ managed by National Center for Seismology, Government of India. The bigger stars are seismicity of magnitude 3.0 ≤ M ≤ 5.1. DSR: Delhi Sargodha Ridge; DHR: Delhi Hardwar Ridge; MR1: Medium Resistor 1; MDF: Mahendragarh Dehradun Fault; MR2: Medium Resistor 2; R1: Resistor 1; R2: Resistor R2. The beach ball (B1) suggests a NE striking steep dipping reverse fault motion; the beach ball (B2) suggests a NW striking reverse with strike-slip fault motion and the beach ball (B3) suggests an NNE striking, normal with strike-slip fault motion.