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A steeply-inclined trajectory for the Chicxulub impact

Autor: Collins, G. S., Patel, N., Davison, T. M., Rae, A. S. P., Morgan, J. V., Gulick, S. P. S., Christeson, G. L., Chenot, E., Claeys, P., Cockell, C. S., Coolen, M. J. L., Ferrière, L., Gebhardt, C., Goto, K., Jones, H., Kring, D. A., Lofi, J., Lowery, C. M., Ocampo-Torres, R., Perez-Cruz, L., Pickersgill, A. E., Poelchau, M. H., Rasmussen, C., Rebolledo-Vieyra, M., Riller, U., Sato, H., Smit, J., Tikoo, S. M., Tomioka, N., Urrutia-Fucugauchi, J., Whalen, M. T., Wittmann, A., Xiao, L., Yamaguchi, K. E., Artemieva, N., Bralower, T. J.

Publikováno v: IODP-ICDP Expedition 364 Science Party & Third-Party Scientists 2020, ' A steeply-inclined trajectory for the Chicxulub impact ', Nature Communications, vol. 11, no. 1, 1480 . https://doi.org/10.1038/s41467-020-15269-x
Nature Communications, 11(1):1480. Nature Publishing Group
Nature Communications
Nature Communications, Nature Publishing Group, 2020, 11 (1), ⟨10.1038/s41467-020-15269-x⟩
Nature Communications, Vol 11, Iss 1, Pp 1-10 (2020)

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.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3e3b2da5b2cc7ed752bf3755fc9ee18
https://research.vu.nl/en/publications/954188eb-9137-4e1b-aa49-ba9a755e4c45

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

Constraining the Decline of the Lunar Dynamo Field at ≈3.1 Ga Through Paleomagnetic Analyses of Apollo 12 Mare Basalts.

Autor: Strauss, B. E.^1,2 beck.strauss@nist.gov, Tikoo, S. M.^1,3, Gross, J.^1,4,5, Setera, J. B.^1,6, Turrin, B.¹

Publikováno v: Journal of Geophysical Research. Planets. Mar2021, Vol. 126 Issue 3, p1-21. 21p.