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Nomograms for rapid evaluation of magnetic anomalies over long tabular bodies

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Abstract

The magnetic anomaly due to a long tabular body usually consists of a maximum and a minimum. The distances and the amplitudes of the maximum and the minimum, when defined in dimensionless quantities, may be used as characteristics of the source. In this paper, a method based on the positions of the maximum and the minimum on the magnetic anomaly due to a long tabular body has been presented. Characteristic ratios,D andA involving the distances and amplitudes of the maximum and the minimum points on the anomaly curve are defined. Nomograms showing the variations ofD andA with the parameters of (1) the dike and (2) the vertical fault models are presented. The parameters of the causative source are evaluated from the two ratiosD andA and the nomograms, using some simple analytical relations presented here. From the nomograms, it is observed that (a) for a thick dike,A is always greater thanD, (b)A=D for a thin sheet and (c) for a vertical fault,A is always less thanD. Thus from the characteristic ratiosD andA it is possible to evaluate the source parameters and also to distinguish whether the source is a dike, sheet or a vertical fault. The method is fast and is applicable for the magnetic anomalies either in total, vertical or horizontal component. The method has been applied on two field examples and the results are found to be in close agreement with those obtained by using other methods. A simple method of locating the origin on the anomaly curve is included. The limitations of the method are also discussed.

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References

  • Am, K. (1972),The Arbitrarily Magnetized Dike: Interpretation by Characteristics, Geoexploration10, 63–90.

    Google Scholar 

  • Bean, R. J. (1966),A Rapid Graphical Solution for the Aeromagnetic Anomaly of the Two-Dimensional Tabular Body, Geophysics31, 963–970.

    Google Scholar 

  • Bruckshaw, J. M., andKunaratnam, K. (1963),The Interpretation of Magnetic Anomalies Due to Dykes, Geophys. Prospect.11, 509–522.

    Google Scholar 

  • Gay, S. P. (1963),Standard Curves for Interpretation of Magnetic Anomalies Over Long Tabular Bodies, Geophysics28, 161–200.

    Google Scholar 

  • Grant, F. S., andMartin, L. (1966),Interpretation of Aeromagnetic Anomalies by the Use of Characteristic Curves, Geophysics31, 135–148.

    Google Scholar 

  • Hood, P. (1964),The Königsberger Ratio and the Dipping-Dike Equation, Geophys. Prospect.12, 440–456.

    Google Scholar 

  • Koulomzine, Th., Lamontagne, Y., andNadeau, A. (1970),New Methods for the Direct Interpretation of Magnetic Anomalies Caused by Inclined Dikes of Infinite Length, Geophysics,35, 812–830.

    Google Scholar 

  • Moo, J. K. C. (1965),Analytical Aeromagnetic Interpretation: The Inclined Prism, Geophys. Prospect.13, 203–224.

    Google Scholar 

  • Powell, D. W. (1967),Fitting Observed Profiles to a magnetized Dike or Fault-Step Model, Geophys. Prospect.15, 208–220.

    Google Scholar 

  • Qureshi, I. R., andNalaye, A. M. (1978),A Method for the Direct Interpretation of Magnetic Anomalie. Caused by Two-Dimensional Vertical Faults, Geophysics43, 179–188.

    Google Scholar 

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Rao, D.A., Ram Babu, H.V. Nomograms for rapid evaluation of magnetic anomalies over long tabular bodies. PAGEOPH 119, 1037–1050 (1981). https://doi.org/10.1007/BF00878968

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  • DOI: https://doi.org/10.1007/BF00878968

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