1. Extraordinary rocks from the peak ring of the Chicxulub impact crater: P-wave velocity, density, and porosity measurements from IODP/ICDP Expedition 364
- Author
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Jaime Urrutia-Fucugauchi, Axel Wittmann, C. Mellett, Kosei E. Yamaguchi, David A. Kring, Honami Sato, Ludovic Ferrière, Mario Rebolledo-Vieyra, Johanna Lofi, Rubén Ocampo-Torres, Cornelia Rasmussen, Auriol S. P. Rae, Marco J. L. Coolen, Heather L. Jones, Michael H. Poelchau, Long Xiao, Annemarie E. Pickersgill, Michael T. Whalen, Philippe Claeys, Kazuhisa Goto, Naotaka Tomioka, Ulrich Riller, Timothy J. Bralower, Chris Nixon, Christopher M. Lowery, S. Green, Elise Chenot, Jan Smit, Sonia M. Tikoo, Douglas R. Schmitt, Ligia Pérez-Cruz, E. Le Ber, Joanna Morgan, Sean P. S. Gulick, Charles S. Cockell, Gail L. Christeson, Catalina Gebhardt, Institute for Geophysics, University of Texas at Austin [Austin], Department of Geological Sciences, Department of Earth Science and Engineering, Imperial College London, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research ( AWI ), Lunar and Planetary Institute [Houston] ( LPI ), Department of Geology, University of Leicester, Géosciences Montpellier, Institut national des sciences de l'Univers ( INSU - CNRS ) -Université de Montpellier ( UM ) -Université des Antilles ( UA ) -Centre National de la Recherche Scientifique ( CNRS ), Department of Physics, University of Alberta [Edmonton], University of Freiburg [Freiburg], Institut für Geologie, Universität Hamburg ( UHH ), Eyring Materials Center, Arizona State University [Tempe] ( ASU ), Department of Geosciences, PennState University [Pennsylvania] ( PSU ), Biogéosciences [Dijon] ( BGS ), Université de Bourgogne ( UB ) -AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique ( CNRS ), Analytical, Environmental and Geo-Chemistry, Vrije Universiteit [Brussel] ( VUB ), School of Physics and Astronomy, University of Edinburgh, WA-Organic and Isotope Geochemistry Centre ( WA-OIGC ), Curtin University [Perth], Planning and Transport Research Centre ( PATREC ) -Planning and Transport Research Centre ( PATREC ), Natural History Museum [Vienna] ( NHM ), British Geological Survey [Edinburgh], International Research Institute of Disaster Science, Tohoku University [Sendai], United Kingdom Hydrographic Office, Institut de chimie et procédés pour l'énergie, l'environnement et la santé ( ICPEES ), Université de Strasbourg ( UNISTRA ) -Centre National de la Recherche Scientifique ( CNRS ) -Matériaux et nanosciences d'Alsace, Université de Strasbourg ( UNISTRA ) -Université de Haute-Alsace (UHA) Mulhouse - Colmar ( Université de Haute-Alsace (UHA) ) -Institut National de la Santé et de la Recherche Médicale ( INSERM ) -Centre National de la Recherche Scientifique ( CNRS ) -Université de Strasbourg ( UNISTRA ) -Université de Haute-Alsace (UHA) Mulhouse - Colmar ( Université de Haute-Alsace (UHA) ) -Institut National de la Santé et de la Recherche Médicale ( INSERM ) -Centre National de la Recherche Scientifique ( CNRS ), Instituto de Geofísica, Universidad Nacional Autónoma de México ( UNAM ), School of Geographical and Earth Sciences, University of Glasgow, Argon Isotope Facility, NERC/SUERC, Department of Geology and Geophysics, University of Utah, Japan Agency for Marine-Earth Science and Technology ( JAMSTEC ), Faculty of Earth and Life Sciences ( FALW ), Vrije Universiteit Amsterdam [Amsterdam] ( VU ), Earth and Planetary Sciences, Rutgers, The State University of New Jersey [New Brunswick] ( RUTGERS ), Kochi Institute for Core Sample Research, University of Alaska Fairbanks ( UAF ), School of Earth Sciences, China University of Geosciences-Planetary Science Institute, Department of Chemistry, NASA Astrobiology Institute ( NAI ), Funding from the In-ternational Ocean Discovery Program (IODP) and the International Continental scientific Drilling Project (ICDP)., Analytical, Environmental & Geo-Chemistry, Chemistry, Earth System Sciences, Institute of Geophysics [Austin] (IG), Department of Geological Sciences [Austin], Jackson School of Geosciences (JSG), University of Texas at Austin [Austin]-University of Texas at Austin [Austin], Department of Earth Science and Engineering [Imperial College London], Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Lunar and Planetary Institute [Houston] (LPI), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Université des Antilles (UA)-Centre National de la Recherche Scientifique (CNRS), University of Alberta, Universität Hamburg (UHH), Arizona State University [Tempe] (ASU), Pennsylvania State University (Penn State), Penn State System-Penn State System, Biogéosciences [UMR 6282] [Dijon] (BGS), Université de Bourgogne (UB)-AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique (CNRS), Analytical, Environmental and Geo- Chemistry, Vrije Universiteit Brussel (VUB), SUPA School of Physics and Astronomy [Edinburgh], WA-Organic and Isotope Geochemistry Centre (WA-OIGC), The Institute for Geoscience Research [Perth] (TIGeR), School of Earth and Planetary Science [Perth - Curtin university], Planning and Transport Research Centre (PATREC)-Planning and Transport Research Centre (PATREC)-Curtin University [Perth], Planning and Transport Research Centre (PATREC)-Planning and Transport Research Centre (PATREC)-School of Earth and Planetary Science [Perth - Curtin university], Planning and Transport Research Centre (PATREC)-Planning and Transport Research Centre (PATREC), Natural History Museum [Vienna] (NHM), British Geological Survey (BGS), Institut de chimie et procédés pour l'énergie, l'environnement et la santé (ICPEES), Université de Strasbourg (UNISTRA)-Matériaux et nanosciences d'Alsace (FMNGE), Institut de Chimie du CNRS (INC)-Université de Strasbourg (UNISTRA)-Université de Haute-Alsace (UHA) Mulhouse - Colmar (Université de Haute-Alsace (UHA))-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC)-Université de Strasbourg (UNISTRA)-Université de Haute-Alsace (UHA) Mulhouse - Colmar (Université de Haute-Alsace (UHA))-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Universidad Nacional Autónoma de México (UNAM), NERC Argon Isotope Facility [Glasgow], Scottish Universities Environmental Research Centre (SUERC), University of Glasgow-University of Edinburgh-University of Glasgow-University of Edinburgh-Natural Environment Research Council (NERC), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Faculty of Earth and Life Sciences [Amsterdam] (FALW), Vrije Universiteit Amsterdam [Amsterdam] (VU), Department of Earth and Planetary Sciences [Piscataway], Rutgers, The State University of New Jersey [New Brunswick] (RU), Rutgers University System (Rutgers)-Rutgers University System (Rutgers), University of Alaska [Fairbanks] (UAF), School of Earth Sciences [Wuham], China University of Geosciences [Wuhan] (CUG), NASA Astrobiology Institute (NAI), and Geology and Geochemistry
- Subjects
Geochemistry & Geophysics ,010504 meteorology & atmospheric sciences ,[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] ,Lithology ,04 Earth Sciences ,Borehole ,Stratigraphic unit ,010502 geochemistry & geophysics ,[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,01 natural sciences ,physical properties ,[ SDU.STU.GP ] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] ,Impact crater ,Geochemistry and Petrology ,Breccia ,Earth and Planetary Sciences (miscellaneous) ,SDG 14 - Life Below Water ,Petrology ,Porosity ,0105 earth and related environmental sciences ,Chicxulub peak ring physical properties impact crater ,02 Physical Sciences ,Scientific drilling ,impact crater ,peak ring ,Geophysics ,Chicxulub ,Space and Planetary Science ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Sedimentary rock ,Geology - Abstract
Joint International Ocean Discovery Program and International Continental Scientific Drilling Program Expedition 364 drilled into the peak ring of the Chicxulub impact crater. We present P-wave velocity, density, and porosity measurements from Hole M0077A that reveal unusual physical properties of the peak-ring rocks. Across the boundary between post-impact sedimentary rock and suevite (impact melt-bearing breccia) we measure a sharp decrease in velocity and density, and an increase in porosity. Velocity, density, and porosity values for the suevite are 2900–3700 m/s, 2.06–2.37 g/cm3, and 20–35%, respectively. The thin (25 m) impact melt rock unit below the suevite has velocity measurements of 3650–4350 m/s, density measurements of 2.26–2.37 g/cm3, and porosity measurements of 19–22%. We associate the low velocity, low density, and high porosity of suevite and impact melt rock with rapid emplacement, hydrothermal alteration products, and observations of pore space, vugs, and vesicles. The uplifted granitic peak ring materials have values of 4000–4200 m/s, 2.39–2.44 g/cm3, and 8–13% for velocity, density, and porosity, respectively; these values differ significantly from typical unaltered granite which has higher velocity and density, and lower porosity. The majority of Hole M0077A peak-ring velocity, density, and porosity measurements indicate considerable rock damage, and are consistent with numerical model predictions for peak-ring formation where the lithologies present within the peak ring represent some of the most shocked and damaged rocks in an impact basin. We integrate our results with previous seismic datasets to map the suevite near the borehole. We map suevite below the Paleogene sedimentary rock in the annular trough, on the peak ring, and in the central basin, implying that, post impact, suevite covered the entire floor of the impact basin. Suevite thickness is 100–165 m on the top of the peak ring but 200 m in the central basin, suggesting that suevite flowed downslope from the collapsing central uplift during and after peak-ring formation, accumulating preferentially within the central basin.
- Published
- 2018
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