The amplitude and phase of the derivatives of the magnetic anomalies of thin dykes and contacts
Gordon R. J. CooperSchool of Geosciences, University of the Witwatersrand, Johannesburg 2050, South Africa. Email: gordon.cooper@wits.ac.za
Exploration Geophysics 47(4) 290-295 https://doi.org/10.1071/EG16012
Submitted: 3 February 2016 Accepted: 3 May 2016 Published: 10 June 2016
Abstract
If the horizontal and vertical derivatives of the total field magnetic anomalies of thin dykes and contacts (and the magnetic anomaly from a thin dyke) are put into an amplitude-phase form, then this can aid in their interpretation. First, it allows derivatives of fractional order to be calculated analytically; second, estimates of the source dip can be made; and finally, the relationships between local wavenumber and source-distance semi-automatic interpretation methods are clarified. The approach is demonstrated on synthetic data and aeromagnetic data from South Africa.
Key words: magnetics, semiautomatic interpretation, potential fields.
References
Cooper, G. R. J., 2014a, Euler deconvolution in a radial coordinate system: Geophysical Prospecting, 62, 1169–1179| Euler deconvolution in a radial coordinate system:Crossref | GoogleScholarGoogle Scholar |
Cooper, G. R. J., 2014b, The automatic determination of the location and depth of contacts and dykes from aeromagnetic data: Pure and Applied Geophysics, 171, 2417–2423
| The automatic determination of the location and depth of contacts and dykes from aeromagnetic data:Crossref | GoogleScholarGoogle Scholar |
Cooper, G. R. J., 2015, Using the analytic signal amplitude to determine the location and depth of thin dykes from magnetic data: Geophysics, 80, J1–J6
| Using the analytic signal amplitude to determine the location and depth of thin dykes from magnetic data:Crossref | GoogleScholarGoogle Scholar |
Cooper, G. R. J., and Cowan, D. R., 2003, The application of fractional calculus to potential field data: Exploration Geophysics, 34, 51–56
| The application of fractional calculus to potential field data:Crossref | GoogleScholarGoogle Scholar |
Cooper, G. R. J., and Whitehead, R. C., 2016, Determining the distance to magnetic sources: Geophysics, 81, J39–J48
| Determining the distance to magnetic sources:Crossref | GoogleScholarGoogle Scholar |
Florio, G., Fedi, M., and Pasteka, R., 2006, On the application of Euler deconvolution to the analytic signal: Geophysics, 71, L87–L93
| On the application of Euler deconvolution to the analytic signal:Crossref | GoogleScholarGoogle Scholar |
Hsu, S.-K., Sibuet, J.-C., and Shyu, C.-T., 1996, High-resolution detection of geologic boundaries from potential field anomalies: an enhanced analytic signal technique: Geophysics, 61, 373–386
| High-resolution detection of geologic boundaries from potential field anomalies: an enhanced analytic signal technique:Crossref | GoogleScholarGoogle Scholar |
Misral, S., and Andreoli, M. A. G., 2012. Post-impact dolerite dykes in the ~145 Ma Morokweng Crater, South Africa: impact related? 43rd Lunar and Planetary Science Conference, 1–4.
Nabighian, M. N., 1972, The analytical signal of 2D magnetic bodies with polygonal cross-section: its properties and use for automated anomaly interpretation: Geophysics, 37, 507–517
| The analytical signal of 2D magnetic bodies with polygonal cross-section: its properties and use for automated anomaly interpretation:Crossref | GoogleScholarGoogle Scholar |
Reford, M. S., 1964, Magnetic anomalies over thin sheets: Geophysics, 29, 532–536
| Magnetic anomalies over thin sheets:Crossref | GoogleScholarGoogle Scholar |
Reid, A. B., Allsop, J. M., Granser, H., Millet, A. J., and Somerton, I. W., 1990, Magnetic interpretation in three dimensions using Euler deconvolution: Geophysics, 55, 80–91
| Magnetic interpretation in three dimensions using Euler deconvolution:Crossref | GoogleScholarGoogle Scholar |
Salem, A., Ravat, D., Smith, R. S., and Ushijima, K., 2005, Interpretation of magnetic data using an enhanced local wavenumber (ELW) method: Geophysics, 70, L7–L12
| Interpretation of magnetic data using an enhanced local wavenumber (ELW) method:Crossref | GoogleScholarGoogle Scholar |
Salem, A., Williams, S., Fairhead, J. D., Ravat, D., and Smith, R. S., 2007, Tilt-depth method: a simple depth estimation method using first-order magnetic derivatives: The Leading Edge, 26, 1502–1505
| Tilt-depth method: a simple depth estimation method using first-order magnetic derivatives:Crossref | GoogleScholarGoogle Scholar |
Taner, M. T., Koehler, F., and Sheriff, R. E., 1979, Complex seismic trace analysis: Geophysics, 44, 1041–1063
| Complex seismic trace analysis:Crossref | GoogleScholarGoogle Scholar |
Thompson, D. T., 1982, Euldph: a new technique for making computer assisted depth estimates from magnetic data: Geophysics, 47, 31–37
| Euldph: a new technique for making computer assisted depth estimates from magnetic data:Crossref | GoogleScholarGoogle Scholar |
Thurston, J. B., and Smith, R. S., 1997, Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI method: Geophysics, 62, 807–813
| Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI method:Crossref | GoogleScholarGoogle Scholar |