Site M0077: Lower Peak Ring

dc.contributor.author Morgan, Joanna V.
dc.contributor.author Gulick, Sean P. S.
dc.contributor.author Mellett, Claire L.
dc.contributor.author Green, S. L.
dc.contributor.author Kring, David A. (David Allen)
dc.contributor.author https://orcid.org/0000-0002-3440-6282
dc.coverage.spatial Mexico
dc.date.accessioned 2020-05-26T22:03:05Z
dc.date.available 2020-05-26T22:03:05Z
dc.date.issued 2017-12-30
dc.description.abstract From 747.02 meters below seafloor (mbsf) to the base of Hole M0077A at 1334.69 mbsf, granitoids intruded by pre-impact mafic and felsic dikes were recovered, interspersed with suevite and impact melt rock (Core 95R-3, 117 cm, through Core 303R at the base of hole). The following sections detail the data and measurements from this Lower Peak Ring interval. 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 Pages 1-26
dc.format.mimetype application/pdf
dc.identifier.other https://doi.org/10.14379/iodp.proc.364.107.2017
dc.identifier.uri https://hdl.handle.net/20.500.11753/1545
dc.language.iso en en
dc.publisher International Ocean Discovery Program en
dc.relation.ispartofseries LPI contribution ; no. 2079
dc.rights.license This work is distributed under the Creative Commons Attribution 4.0 International (CC BY 4.0) license
dc.subject Cretaceous-Paleogene boundary en
dc.subject Chicxulub Crater en
dc.title Site M0077: Lower Peak Ring en
dc.type Article en
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