Imperial College London
Portrait Picture

Professor Gareth Collins

Faculty of Engineering, Department of Earth Science & Engineering

Professor of Planetary Science
 
 
 
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Contact

 

+44 (0)20 7594 1518g.collins Website

 
 
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Location

 

4.83Royal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Urrutia-Fucugauchi:2019:10.1111/gto.12261,
author = {Urrutia-Fucugauchi, J and Pérez-Cruz, L and Morgan, J and Gulick, S and Wittmann, A and Lofi, J and Morgan, JV and Gulick, SPS and Chenot, E and Christeson, G and Claeys, P and Cockell, C and Coolen, MJL and Ferrière, L and Gebhardt, C and Goto, K and Jones, H and Kring, DA and Lofi, J and Lowery, C and Mellett, C and Ocampo-Torres, R and Perez-Cruz, L and Pickersgill, A and Poelchau, M and Rae, A and Rasmussen, C and Rebolledo-Vieyra, M and Riller, U and Sato, H and Smit, J and Tikoo-Schantz, S and Tomioka, N and Urrutia-Fucugauchi, J and Whalen, M and Wittmann, A and Xiao, L and Yamaguchi, KE and Bralower, T and Collins, GS},
doi = {10.1111/gto.12261},
journal = {Geology Today},
pages = {68--72},
title = {Peering inside the peak ring of the Chicxulub Impact Crater—its nature and formation mechanism},
url = {http://dx.doi.org/10.1111/gto.12261},
volume = {35},
year = {2019}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - © 2019 John Wiley  &  Sons Ltd, The Geologists' Association  &  The Geological Society of London The IODP-ICDP Expedition 364 drilled into the Chicxulub crater, peering inside its well-preserved peak ring. The borehole penetrated a sequence of post-impact carbonates and a unit of suevites and clast-poor impact melt rock at the top of the peak ring. Beneath this sequence, basement rocks cut by pre-impact and impact dykes, with breccias and melt, were encountered at shallow depths. The basement rocks are fractured, shocked and uplifted, consistent with dynamic collapse, uplift and long-distance transport of weakened material during collapse of the transient cavity and final crater formation.
AU  - Urrutia-Fucugauchi,J
AU  - Pérez-Cruz,L
AU  - Morgan,J
AU  - Gulick,S
AU  - Wittmann,A
AU  - Lofi,J
AU  - Morgan,JV
AU  - Gulick,SPS
AU  - Chenot,E
AU  - Christeson,G
AU  - Claeys,P
AU  - Cockell,C
AU  - Coolen,MJL
AU  - Ferrière,L
AU  - Gebhardt,C
AU  - Goto,K
AU  - Jones,H
AU  - Kring,DA
AU  - Lofi,J
AU  - Lowery,C
AU  - Mellett,C
AU  - Ocampo-Torres,R
AU  - Perez-Cruz,L
AU  - Pickersgill,A
AU  - Poelchau,M
AU  - Rae,A
AU  - Rasmussen,C
AU  - Rebolledo-Vieyra,M
AU  - Riller,U
AU  - Sato,H
AU  - Smit,J
AU  - Tikoo-Schantz,S
AU  - Tomioka,N
AU  - Urrutia-Fucugauchi,J
AU  - Whalen,M
AU  - Wittmann,A
AU  - Xiao,L
AU  - Yamaguchi,KE
AU  - Bralower,T
AU  - Collins,GS
DO  - 10.1111/gto.12261
EP  - 72
PY  - 2019///
SN  - 0266-6979
SP  - 68
TI  - Peering inside the peak ring of the Chicxulub Impact Crater—its nature and formation mechanism
T2  - Geology Today
UR  - http://dx.doi.org/10.1111/gto.12261
VL  - 35
ER  -
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