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The Habitat of the Nascent Chicxulub Crater

Abstract An expanded sedimentary section provides an opportunity to elucidate conditions in the nascent Chicxulub crater during the hours to millennia after the Cretaceous‐Paleogene (K‐Pg) boundary impact. The sediments were deposited by tsunami followed by seiche waves as energy in the crater decli...

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Bibliografische gegevens
Hoofdauteurs: T. J. Bralower, J. Cosmidis, M. S. Fantle, C. M. Lowery, B. H. Passey, S. P. S. Gulick, J. V. Morgan, V. Vajda, M. T. Whalen, A. Wittmann, N. Artemieva, K. Farley, S. Goderis, E. Hajek, P. J. Heaney, D. A. Kring, S. L. Lyons, C. Rasmussen, E. Sibert, F. J. Rodríguez Tovar, G. Turner‐Walker, J. C. Zachos, J. Carte, S. A. Chen, C. Cockell, M. Coolen, K. H. Freeman, J. Garber, M. Gonzalez, J. L. Gray, K. Grice, H. L. Jones, B. Schaefer, J. Smit, S. M. Tikoo
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Wiley 2020-12-01
Reeks:AGU Advances
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Online toegang:https://doi.org/10.1029/2020AV000208
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