Abstract
Data from surface, aerostat (balloon), and satellite surveys were used in constructing profiles of the anomalous magnetic field of Siberia. Wavelet analysis of the profiles revealed a number of longitude inhomogeneities in the structure of anomalous magnetic fields. It is shown that the dynamics of anomalous fields is concentrated for the most part in the range of low values of the wavelet transformation scale factors. Good agreement between the estimates of depths to the sources on the basis of magnetic data and information on heat-flow distribution facilitates an understanding of the tectonic structure of this region.
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.
