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Winding down the Chicxulub impact: The transition between impact and normal marine sedimentation near ground zero

Autor: Whalen, Michael, Gulick, Sean P.S., Lowery, Christopher, Bralower, Timothy, Morgan, Joanna, Grice, Kliti, Schaefer, Bettina, Smit, Jan, Ormö, Jens, Wittmann, Axel, Kring, David, Lyons, Shelby, Goderis, Steven, Chenot, Elise, Christeson, Gail l., Clayes, Philippe, Cockell, Charles S., Coolen, Marco, Gebhardt, Catalina, Goto, Kazuhisa, Jones, Heather, LOFI, Johanna, IODP-ICDP Expedition 364 scientists,, Perez-Cruz, Ligia, Pickersgill, Annemarie E., Poelchau, Michael H., Rae, A.S.P., Green, Sophie L., Rasmussen, Cornelia, Sato, Honami, Tikoo, Sonia, Tomioka, Naotaka, Urrutia Fucugauchi, Jaime, Xiao, Long, Yamaguchi, Kosei E.

Publikováno v: DIGITAL.INTA Repositorio Digital del Instituto Nacional de Técnica Aeroespacial
instname
Marine Geology, 430:106368, 1-18. Elsevier
Marine Geology
Marine Geology, Elsevier, 2020, 430, pp.106368. ⟨10.1016/j.margeo.2020.106368⟩
Digital.CSIC. Repositorio Institucional del CSIC
Instituto Nacional de Técnica Aeroespacial (INTA)
Whalen, M T, Gulick, S P S, Lowery, C M, Bralower, T J, Morgan, J V, Grice, K, Schaefer, B, Smit, J, Ormö, J, Wittmann, A, Kring, D A, Lyons, S & Goderis, S 2020, ' Winding down the Chicxulub impact : The transition between impact and normal marine sedimentation near ground zero ', Marine Geology, vol. 430, 106368, pp. 1-18 . https://doi.org/10.1016/j.margeo.2020.106368

IODP-ICDP Expedition 364 Scientists complete list of expedition scientists is in Appendix A.
The Chicxulub impact led to the formation of a ~ 200-km wide by ~1-km deep crater on México's Yucatán Peninsula. Over a period of hours after the impa

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53dd2a17780f9908753a2d9bcf7d0de4
http://hdl.handle.net/20.500.12666/248

Stress‐Strain Evolution During Peak‐Ring Formation: A Case Study of the Chicxulub Impact Structure

Autor: Rae, Auriol, Collins, Gareth, Poelchau, Michael, Riller, Ulrich, Davison, Thomas, Grieve, Richard, Osinski, Gordon, Morgan, Joanna, Gulick, S. P. S., Chenot, Elise, Christeson, G. L., Claeys, P., Cockell, C. S., Coolen, M. J. L., Ferrière, L., Gebhardt, C., Goto, K., Green, S., Jones, H., Kring, D. A., Lofi, Johanna, Lowery, C. M., Ocampo‐Torres, R., Perez‐Cruz, L., Pickersgill, A. E., Rasmussen, C., Rae, A.S.P., Rebolledo‐Vieyra, M., Sato, H., Smit, J., Tikoo, S. M., Tomioka, N., Urrutia‐Fucugauchi, J., Whalen, M. T., Wittmann, A., Xiao, L., Yamaguchi, K. E.

Publikováno v: Journal of Geophysical Research. Planets
Journal of Geophysical Research. Planets, Wiley-Blackwell, 2019, 124 (2), pp.396-417. ⟨10.1029/2018JE005821⟩
2019, ' Stress-Strain Evolution During Peak-Ring Formation : A Case Study of the Chicxulub Impact Structure ', Journal of Geophysical Research: Planets, vol. 124, no. 2, pp. 396-417 . https://doi.org/10.1029/2018JE005821

Deformation is a ubiquitous process that occurs to rocks during impact cratering; thus, quantifying the deformation of those rocks can provide first-order constraints on the process of impact cratering. Until now, specific quantification of the condi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::877ae57191870dc2ea8869bbc20af061
https://hal.umontpellier.fr/hal-02128150/file/Rae_et_al-2019-Journal_of_Geophysical_Research__Planets.pdf

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