Inversion of satellite magnetic anomaly data
Item
Title (Dublin Core)
en-US
Inversion of satellite magnetic anomaly data
Description (Dublin Core)
en-US
A method of finding a first approximation to a crustal magnetization distribution from inversion of satellite magnetic anomaly data is described. Magnetization is expressed as a Fourier series in a segment of spherical shell. Input to this procedure is an equivalent source representation of the observed anomaly field. Instability of the inversion occurs when high frequency noise is present in the input data, or when the series is carried to an excessively high wave number. Preliminary results are given for the United States and adjacent areas.
ARK: https://n2t.net/ark:/88439/y090977
Permalink: https://geophysicsjournal.com/article/159
ARK: https://n2t.net/ark:/88439/y090977
Permalink: https://geophysicsjournal.com/article/159
Creator (Dublin Core)
Mayhew, M.A.
Subject (Dublin Core)
en-US
Magnetic anomalies
en-US
Crustal magnetization
en-US
Equivalent source
en-US
Methods
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1978-12-22
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/159
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 45 No 1 (1978): Journal of Geophysics; 119-128
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/159/119