GEOPHYSICAL CHARACTERIZATION OF THE CHICXULUB IMPACT CRATER

@article{Gulick2013GEOPHYSICALCO,
  title={GEOPHYSICAL CHARACTERIZATION OF THE CHICXULUB IMPACT CRATER},
  author={Sean P. S. Gulick and Gail L. Christeson and Penny J. Barton and Richard A. F. Grieve and J. V. Morgan and Jamie Urrutia-Fucugauchi},
  journal={Reviews of Geophysics},
  year={2013},
  volume={51},
  pages={31 - 52}
}
Geophysical data indicate that the 65.5 million years ago Chicxulub impact structure is a multi‐ring basin, with three sets of semicontinuous, arcuate ring faults and a topographic peak ring (PR). Slump blocks define a terrace zone, which steps down from the inner rim into the annular trough. Fault blocks underlie the PR, which exhibits variable relief, due to target asymmetries. The central structural uplift is >10 km, and the Moho is displaced by 1–2 km. The working hypothesis for the… 
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References

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