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A steeply-inclined trajectory for the Chicxulub impact

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dc.contributor.author Collins, Gareth S.
dc.contributor.author Patel, N.
dc.contributor.author Davison, Thomas M.
dc.contributor.author Rae, A. S. P.
dc.contributor.author Morgan, Joanna V.
dc.contributor.author Gulick, Sean P. S.
dc.contributor.author Kring, David A. (David Allen)
dc.coverage.spatial Mexico
dc.date.accessioned 2020-05-26T19:26:53Z
dc.date.available 2020-05-26T19:26:53Z
dc.date.issued 2020-05-26
dc.identifier.citation Collins, G.S., Patel, N., Davison, T.M. et al. A steeply-inclined trajectory for the Chicxulub impact. Nat Commun 11, 1480 (2020). https://doi.org/10.1038/s41467-020-15269-x en
dc.identifier.other https://doi.org/10.1038/s41467-020-15269-x
dc.identifier.uri https://hdl.handle.net/20.500.11753/1542
dc.description.abstract 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 (<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. en
dc.description.statementofresponsibility G. S. Collins, N. Patel, T. M. Davison, A. S. P. Rae, J. V. Morgan, S. P. S. Gulick, IODP-ICDP Expedition 364 Science Party & Third-Party Scientists
dc.format.extent 10 pages
dc.format.mimetype application/pdf
dc.language.iso en en
dc.publisher Nature en
dc.relation.ispartofseries LPI contribution ; no. 2367
dc.rights This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
dc.subject Chicxulub Crater en
dc.subject Impact en
dc.title A steeply-inclined trajectory for the Chicxulub impact en
dc.type Article en


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