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Expedition 364 Summary

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dc.contributor.author Gulick, Sean
dc.contributor.author Morgan, Joanna
dc.contributor.author Mellett, Claire L.
dc.contributor.author Green, S. L.
dc.contributor.author Kring, David A. (David Allen)
dc.coverage.spatial Mexico
dc.date.accessioned 2020-05-27T20:47:35Z
dc.date.available 2020-05-27T20:47:35Z
dc.date.issued 2017-12-30
dc.identifier.other https://doi.org/10.14379/iodp.proc.364.101.2017
dc.identifier.uri https://hdl.handle.net/20.500.11753/1551
dc.description.abstract During International Ocean Discovery Program (IODP) and International Continental Scientific Drilling Program (ICDP) Expedition 364, Paleogene sedimentary rocks and lithologies that make up the Chicxulub peak ring were cored to investigate (1) the nature and formational mechanism of peak rings, (2) how rocks are weakened during large impacts, (3) the nature and extent of post-impact hydrothermal circulation, (4) the deep biosphere and habitability of the peak ring, and (5) the recovery of life in a sterile zone. en
dc.description.statementofresponsibility S. Gulick, J. Morgan, C.L. Mellett, S.L. Green, T. Bralower, E. Chenot, G. Christeson, P. Claeys, C. Cockell, M.J.L. Coolen, L. Ferrière, C. Gebhardt, K. Goto, H. Jones, D. Kring, J. Lofi, C. Lowery, R. Ocampo-Torres, L. Perez-Cruz, A.E. Pickersgill, M. Poelchau, A. Rae, C. Rasmussen, M. Rebolledo-Vieyra, U. Riller, H. Sato, J. Smit, S. Tikoo, N. Tomioka, J. Urrutia-Fucugauchi, M. Whalen, A. Wittmann, K. Yamaguchi, L. Xiao, and W. Zylberman
dc.format.extent 23 pages
dc.format.mimetype application/pdf
dc.language.iso en en
dc.publisher International Ocean Discovery Program en
dc.relation.ispartofseries LPI contribution ; no. 2073
dc.subject Chicxulub Crater en
dc.subject Cretaceous-Paleogene boundary en
dc.title Expedition 364 Summary en
dc.type Book chapter en
dc.rights.license This work is distributed under the Creative Commons Attribution 4.0 International (CC BY 4.0) license


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