Abstract
Wide band magnetotelluric measurements were carried out at 16 sites along Guhaghar–Sangole traverse across the Koyna seismicity zone. The results of the study, besides providing details of Deccan trap thickness variation along the traverse, brought out several structural characteristics of the subsurface extending to deep crustal levels. The Koyna fault zone is characterized by a weak expression of a moderately conductive feature extending only up to a depth of 4–5 km. Two-dimensional modeling results bring out distinct block structure in the Koyna region and are compared with velocity and density structure of the region. The deep electrical structure is interpreted in terms of lateral lithological heterogeneities.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
