Aerial surveys of the Vredefort impact crater in South Africa suggest that it is only weakly magnetic. The rocks themselves tell a different story, but does this apply to giant impact basins on Mars?
References
Acuña, M. H. et al. Science 284, 790–793 (1999).
Hood, L. L., Richmond, N. C., Pierazzo, E. & Rochette, P. Geophys. Res. Lett. 30, 1281 (2003).
Rochette, P., Hood, L. L., Fillion, G., Ballou, R. & Ouladdiaf, B. Eos Trans. Am. Geophys. Un. 84, 561, 567 (2003).
Mohit, P. S. & Arkani-Hamed, J. Icarus 168, 305–317 (2004).
Carporzen, L., Gilder, S. A. & Hart, R. J. Nature 435, 199–201 (2005).
Dunlop, D. J. & Özdemir, Ö. Rock Magnetism: Fundamentals and Frontiers (Cambridge Univ. Press, 1997).
McSween, H. Y., Grove, T. L. & Wyatt, M. B. J. Geophys. Res. 108, 5135 (2003).
Connerney, J. E. P. et al. Science 284, 794–798 (1999).
Dunlop, D. J. & Arkani-Hamed, J. http://www.agu.org/pubs/pip
Fuller, M. Rev. Geophys. Space Phys. 12, 23–70 (1974).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Dunlop, D. Magnetic impact craters. Nature 435, 156–157 (2005). https://doi.org/10.1038/435156a
Published:
Issue Date:
DOI: https://doi.org/10.1038/435156a
- Springer Nature Limited