Abstract
This paper describes method of gravity field interpretation, which is based on the stable algorithm of inversion. Stability of the algorithm is ensured by the selection of initial density model and by step-by-step solution of the problem on the correctness set. We obtain stable and meaningful solution of inverse problem by calculation of small additions from the initial model. Algorithm shows efficiency for the restoration of curvilinear layers. Practical example of interpretation of gravity data is provided for gravity data of Urals region.
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.
