Application of the Hartley Transform to the Interpretation of Magnetic Anomalies Due to Two-Dimensional Dyke Bodies

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dc.contributor.authorMarobhe, Isaac M.
dc.date.accessioned2016-09-21T13:11:11Z
dc.date.available2016-09-21T13:11:11Z
dc.date.issued1990
dc.descriptionFull text can be accessed at http://www.sciencedirect.com/science/article/pii/001671429090009Hen_US
dc.description.abstractThis study deals with the application of the Hartley transform in the inversion of total field magnetic anomalies due to a two-dimensional dyke model. The ratio of the Hartley transform to the amplitude spectrum gives the function from which the centre, magnetisation angle and dip may be determined. The depth and width of the dyke are determined from the amplitude spectrum. Tests using theoretical anomalies have shown that most of the estimates of the parameters are in agreement with parameters used to compute the anomalies. Proper scaling of the transform is required to better estimate depth and intensity of magnetisation.en_US
dc.identifier.citationMarobhe, I.M., 1990. Application of the Hartley transform to the interpretation of magnetic anomalies due to two-dimensional dyke bodies. Geoexploration, 26(4), pp.291-301.en_US
dc.identifier.doi10.1016/0016-7142(90)90009-H
dc.identifier.urihttp://hdl.handle.net/20.500.11810/3879
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.titleApplication of the Hartley Transform to the Interpretation of Magnetic Anomalies Due to Two-Dimensional Dyke Bodiesen_US
dc.typeJournal Article, Peer Revieweden_US
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