Abstract
Determining magnetic parameters of rock samples by means of an astatic magnetometer is essentially solving a certain kind of the inverse problem. If the sample is measured at small distances from the astatic system, or if the sample is magnetically strongly inhomogeneous, the problem of higher order magnetic moments becomes more difficult. The accuracy of estimating the parameters depends on the correctness and the comprehensiveness of the model chosen. In the present paper a statistical model is proposed, which solves satisfactorily the problem of measuring the magnetic parameters of a generally magnetized sample provided the remanent moment distinctly dominates over the induced moment.
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.
