Abstract
Magnetotelluric responses of a 3D inhomogeneous earth excited by an arbitrary EM field are nonlocal, which is essential in processing regional MTS data. Due regard for this effect requires data acquisition by a dense synchronous 2D array. We suggest to invert the nonlocal MT responses applying correlation of the surface telluric and magnetic components recorded simultaneously at all stations. The new inversion algorithm has been tested using synthetic data that reproduce the conditions of the BEAR experiment.
Sign-in/Register to access full text options 
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.
