1887
24th International Geophysical Conference and Exhibition – Geophysics and Geology Together for Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Directly interpreting total-field magnetic anomaly data in the South China Sea (SCS) can be difficult because of the complex patterns associated with low-latitude anomaly projection and the presence of remanent magnetization. Additional difficulty arises from the fact that the ambient field direction, thus, the total-field anomaly projection direction, varies over a wide range in the area. To alleviate these difficulties, we present a strategy by using magnetic amplitude data analyses and inversion. Equivalent source processing is used to calculate the amplitude data in the space domain since the wavenumber-domain method is no longer applicable due to low and highly variable inclination. The amplitude data serve the role of reduction-to-pole (RTP) transformation for structural interpretation. We then carry out the amplitude inversion to generate a 3D subsurface distribution of effective susceptibility. The inversion results show that this approach is feasible and effective in SCS.

Loading

Article metrics loading...

/content/journals/10.1071/ASEG2015ab233
2015-12-01
2026-01-19
Loading full text...

Full text loading...

References

  1. Briais A, Patriat P, and Tapponnier P. 1993, Updated interpretation of magnetic anomalies and seafloor spreading in the South China Sea: implications for the Tertiary Tectonics of Southeast Asia: Geophysical Research, 98(B4): 6299-6328.
  2. Dampney, C. N. G., 1969, The equivalent source technique: Geophysics, 34, 38-53.
  3. Dannemiller, N., and Li, Y., 2006, A new method for estimation of magnetization direction: Geophysics, 71(6), L69-L73.
  4. Dransfield, M., A. Christensen, and Liu, G. 2003, Airborne vector magnetics mapping of remanently magnetized banded iron formations at Rocklea, Western Australia: Exploration Geophysics, 34, 93-96.
  5. Gerovska D., Arauzo-Bravo M J., Stavrev P., 2009, Estimating the magnetization direction of sources from southeast Bulgaria through correlation between reduced-to-the-pole and total magnitude anomalies: Geophysical Prospecting, 57(4), 491505.
  6. Hao, T., Xu, Y., Zhao, B., et al., 2009, Geophysical research on distribution features of magnetic basements in the South China Sea: Chinese journal of geophysics, 52(11), 2763-2776.
  7. Lelievre, P. G., and D.W. Oldenburg, 2009, A3D total magnetization inversion applicable when significant, complicated remanence is present: Geophysics, 74(3), L21-L30.
  8. Li, J., Ding, W., Gao, J., etal.,2011, Cenozoic evolution model of the sea floor spreading in South China Sea: new constraints from high resolution geophysical data: Chinese journal of geophysics, 54(12), 3004-3015.
  9. Li, Y., Shearer S., Haney M., et al. 2010, Comprehensive approaches to 3D inversion of magnetic data affected by remanent magnetization: Geophysics, 75(1), L1-L11.
  10. Li, S., and Li, Y., 2014, Inversion of magnetic anomaly on rugged observation surface in the presence of strong remanent magnetization, Geophysics, 79(2), J11-J19.
  11. Pedersen, L. B., 1978, Wavenumber domain expressions for potential fields from arbitrary 2-, 212 -, and 3-dimensional bodies: Geophysics, 43,626-630.
  12. Phillips, J. D., 2005, Can we estimate total magnetization directions from aeromagnetic data using Helbig’s formulas: Earth, Planets, and Space, 57,681-689.
  13. Shearer, S., 2005, Three-dimensional inversion of magnetic data in the presence of remanent magnetization: M.S. thesis, Colorado School of Mines.
  14. Yao, B., Wan, L., Zeng, W., et al. 2006, The 3D structure and Evolution of the lithosphere of the South China Sea: Geological Publishing House ( Beijing).
  15. CGEM Software, 2014, AMP3D Software package for the amplitude inversion of magnetic data.
/content/journals/10.1071/ASEG2015ab233
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error