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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>The formation of peak rings in large impact craters.</title>
<creator>Morgan, Joanna V.</creator>
<creator>Gulick, Sean P.S.</creator>
<creator>Bralower, Timothy</creator>
<creator>Chenot, Elise</creator>
<creator>Christeson, Gail</creator>
<creator>Claeys, Philippe</creator>
<creator>Cockell, Charles</creator>
<creator>Collins, Gareth S.</creator>
<creator>Coolen, Marco J.L.</creator>
<creator>Ferrière, Ludovic</creator>
<creator>Gebhardt, Catalina</creator>
<creator>Goto, Kazuhisa</creator>
<creator>Jones, Heather</creator>
<creator>Kring, David A.</creator>
<creator>Le Ber, Erwan</creator>
<creator>Lofi, Johanna</creator>
<creator>Long, Xiao</creator>
<creator>Lowery, Christopher</creator>
<creator>Mellett, Claire</creator>
<creator>Ocampo-Torres, Rubén</creator>
<creator>Osinski, Gordon R.</creator>
<creator>Perez-Cruz, Ligia</creator>
<creator>Pickersgill, Annemarie</creator>
<creator>Poelchau, Michael</creator>
<creator>Rae, Auriol</creator>
<creator>Rasmussen, Cornelia</creator>
<creator>Rebolledo-Vieyra, Mario</creator>
<creator>Riller, Ulrich</creator>
<creator>Sato, Honami</creator>
<creator>Schmitt, Douglas R.</creator>
<creator>Smit, Jan</creator>
<creator>Tikoo, Sonia</creator>
<creator>Tomioka, Naotaka</creator>
<creator>Urrutia-Fucugauchi, Jaime</creator>
<creator>Whalen, Michael</creator>
<creator>Wittmann, Axel</creator>
<creator>Yamaguchi, Kosei E.</creator>
<creator>Zylberman, William</creator>
<contributor>Department of Earth Science and Technology [Imperial College London] ; Imperial College London</contributor>
<contributor>Institute for Geophysics ; University of Texas at Austin [Austin] - Jackson School of Geosciences</contributor>
<contributor>Department of Geosciences ; PennState University [Pennsylvania] (PSU)</contributor>
<contributor>Biogéosciences [Dijon] (BGS) ; Centre National de la Recherche Scientifique (CNRS) - Université de Bourgogne (UB) - AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement</contributor>
<contributor>Analytical, Environmental and Geo-Chemistry ; Vrije Universiteit [Brussel] (VUB)</contributor>
<contributor>School of Physics and Astronomy [Edinburgh] ; University of Edinburgh</contributor>
<contributor>WA-Organic and Isotope Geochemistry Centre (WA-OIGC) ; Curtin University [Perth] ; Planning and Transport Research Centre (PATREC) - Planning and Transport Research Centre (PATREC)</contributor>
<contributor>Natural History Museum [Vienna] (NHM)</contributor>
<contributor>Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI)</contributor>
<contributor>International Research Institute of Disaster Science ; Tohoku University [Sendai]</contributor>
<contributor>Lunar and Planetary Institute [Houston] (LPI)</contributor>
<contributor>Department of Geology [Leicester] ; University of Leicester</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>School of Earth Sciences ; China University of Geosciences - Planetary Science Institute</contributor>
<contributor>The Lyell Centre ; British Geological Survey</contributor>
<contributor>Institut de chimie et procédés pour l'énergie, l'environnement et la santé (ICPEES) ; Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Department of Physics and Astronomy [London, ON] ; University of Western Ontario (UWO)</contributor>
<contributor>Centre for Planetary Science and Exploration [London, ON] (CPSX) ; University of Western Ontario (UWO)</contributor>
<contributor>Instituto de Geofísica ; Universidad Nacional Autónoma de México (UNAM)</contributor>
<contributor>School of Geographical and Earth Sciences ; University of Glasgow</contributor>
<contributor>Geology ; University of Freiburg [Freiburg]</contributor>
<contributor>Department of Geology and Geophysics ; University of Utah</contributor>
<contributor>Unidad de Ciencias del Agua ; Centro de Investigación Científica de Yucatán</contributor>
<contributor>Institut für Geologie ; Universität Hamburg (UHH)</contributor>
<contributor>Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</contributor>
<contributor>Department of Physics [Edmonton] ; University of Alberta [Edmonton]</contributor>
<contributor>Faculty of Earth and Life Sciences (FALW) ; Vrije Universiteit Amsterdam [Amsterdam] (VU)</contributor>
<contributor>Department of Earth and Planetary Sciences [Piscataway] ; Rutgers, The State University of New Jersey [New Brunswick] (RUTGERS)</contributor>
<contributor>Kochi Institute for Core Sample Research ; Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</contributor>
<contributor>Department of Geosciences ; University of Alaska Fairbanks (UAF)</contributor>
<contributor>Physical Sciences ; Arizona State University [Tempe] (ASU) - LeRoy Eyring Center for Solid State Science</contributor>
<contributor>Department of Chemistry ; Toho University</contributor>
<contributor>NASA Astrobiology Institute (NAI)</contributor>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Work funded by the European Consortium for Ocean Research Drilling (ECORD) and the International Continental Scientific Program, with contributions and logistical support from the Yucatan State Government and Universidad Nacional Autónoma de México (UNAM).</contributor>
<description>6 pages</description>
<description>International audience</description>
<source>ISSN: 0036-8075</source>
<source>EISSN: 1095-9203</source>
<source>Science</source>
<publisher>American Association for the Advancement of Science</publisher>
<identifier>hal-01399386</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01399386</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01399386</source>
<source>Science, American Association for the Advancement of Science, 2016, 354 (6314), pp.878-882. 〈http://science.sciencemag.org.inee.bib.cnrs.fr/content/354/6314/878〉. 〈10.1126/science.aah6561〉</source>
<identifier>PUBMED : 27856906</identifier>
<relation>info:eu-repo/semantics/altIdentifier/pmid/27856906</relation>
<identifier>DOI : 10.1126/science.aah6561</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1126/science.aah6561</relation>
<source>http://science.sciencemag.org.inee.bib.cnrs.fr/content/354/6314/878</source>
<language>en</language>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Large impacts provide a mechanism for resurfacing planets through mixing near-surface rocks with deeper material. Central peaks are formed from the dynamic uplift of rocks during crater formation. As crater size increases, central peaks transition to peak rings. Without samples, debate surrounds the mechanics of peak-ring formation and their depth of origin. Chicxulub is the only known impact structure on Earth with an unequivocal peak ring, but it is buried and only accessible through drilling. Expedition 364 sampled the Chicxulub peak ring, which we found was formed from uplifted, fractured, shocked, felsic basement rocks. The peak-ring rocks are cross-cut by dikes and shear zones and have an unusually low density and seismic velocity. Large impacts therefore generate vertical fluxes and increase porosity in planetary crust.</description>
<date>2016-11-18</date>
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