Abstract
Spectral analysis of paleomagnetic directions can be accomplished easily by first mapping the data onto the complex plane and then using a reliable spectral estimator such as Burg's maximum entropy method for complex time series. Paleomagnetic measurements on the Narita bed by Nagata et al. serve to illustrate the procedure. Spectra of paleosecular variation are helpful for resolving historical tendencies toward clockwise and counterclockwise field motions associated with nondipole longitudinal drift.
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.
