A steeply-inclined trajectory for the Chicxulub impact

Gareth Collins, Narissa Patel, Thomas Davison, A. S. P. Rae, J. V. Morgan, Sean Gulick, IODP-ICDP Expedition 364 Science Party, G. L. Christeson, E. Chenot, P. Claeys, C. S. Cockell, M. J. L. Coolen, L. Ferrière, C. Gebhardt, K. Goto, H. Jones, D. A. Kring, J. Lofi, C. M. Lowery, R. Ocampo-TorresL. Perez-Cruz, A. E. Pickersgill, M. H. Poelchau, C. Rasmussen, M. Rebolledo-Vieyra, U. Riller, H. Sato, J. Smit, S. M. Tikoo, N. Tomioka, J. Urrutia-Fucugauchi, M. T. Whalen, A. Wittmann, L. Xiao, K. E. Yamaguchi, Third-Party Scientists, N. Artemieva, T. J. Bralower

Research output: Contribution to journalArticlepeer-review

Abstract

<jats:p>The environmental severity of large impacts on Earth is influenced by their impact trajectory. Impact direction and angle to the target plane affect the volume and depth of origin of vaporized target, as well as the trajectories of ejected material. The asteroid impact that formed the 66 Ma Chicxulub crater had a profound and catastrophic effect on Earth’s environment, but the impact trajectory is debated. Here we show that impact angle and direction can be diagnosed by asymmetries in the subsurface structure of the Chicxulub crater. Comparison of 3D numerical simulations of Chicxulub-scale impacts with geophysical observations suggests that the Chicxulub crater was formed by a steeply-inclined (45–60 to horizontal) impact from the northeast; several lines of evidence rule out a low angle (less than 30) impact. A steeply-inclined impact produces a nearly symmetric distribution of ejected rock and releases more climate-changing gases per impactor mass than either a very shallow or near-vertical impact.
Original languageEnglish
JournalNature Communications
DOIs
Publication statusPublished - 26 May 2020

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  • IODP-ICDP Expedition 364

    Rae, A. (Researcher)

    Project: Research

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