Abstract
Deformation and melting of the crust during the formation of large impact craters must have been important during the Earth's early evolution, but such processes remain poorly understood1. The 1.8-billion-year-old Sudbury structure2 in Ontario, Canada, is greater than 200 km in diameter and preserves a complete impact section, including shocked basement rocks, an impact melt sheet and fallback material3,4. It has generally been thought that the most voluminous impact melts represent the average composition of the continental crust4, but here we show that the melt sheet now preserved as the Sudbury Igneous Complex is derived predominantly from the lower crust. We therefore infer that the hypervelocity impact caused a partial inversion of the compositional layering of the continental crust. Using geochemical data, including platinum-group-element abundances, we also show that the matrix of the overlying clast-laden Onaping Formation represents a mixture of the original surficial sedimentary strata, shock-melted lower crust and the impactor itself.
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References
Melosh, H. J. & Ivanov, B. A. Impact crater collapse. Annu. Rev. Earth Planet Sci. 27, 385–415 (1999)
Krogh, T. E., Davis, D. W. & Corfu, F. in The Geology and Ore Deposits of the Sudbury Structure (eds Pye, E. G. et al.) 431–446 (Ontario Geological Survey, Special Vol. 1, 1984)
Dietz, R. S. Sudbury Structure as an astrobleme. J. Geol. 72, 412–434 (1964)
Grieve, R. A. F., Stoffler, D. & Deutsch, A. The Sudbury structure: controversial or misunderstood? J. Geophys. Res. 96, 22,753–22,764 (1991)
Bunch, T. E. et al. in Large Impacts and Planetary Evolution (eds Dressler, B. O. & Sharpton, V. L.) 331–343 (Geological Society of America, Special Paper Vol. 339, 1999)
Ripley, E. M., Park, Y.-R., Lambert, D. D. & Frick, L. R. Re-Os isotopic variations in carbonaceous pelites hosting the Duluth Complex: Implications for metamorphic and metasomatic processes associated with mafic magma chambers. Geochim. Cosmochim. Acta 65, 2965–2978 (2001)
Schneider, D. A., Bickford, M. E., Cannon, W. F., Schulz, K. J. & Hamilton, M. A. Age of volcanic rocks and syndepositional iron formations, Marquette Range Supergroup: implications for the tectonic setting of Paleoproterozoic iron formations of the Lake Superior region. Can. J. Earth Sci. 39, 999–1012 (2002)
Masaitis, V. L. et al. in Large Impacts and Planetary Evolution (eds Dressler, B. O. & Sharpton, V. L.) 317–321 (Geological Society of America, Special Paper Vol. 339, 1999)
Grieve, R. A. F. & Cintala, M. J. An analysis of differential impact melt-crater scaling and implications for the terrestrial impact record. Meteoritics 27, 526–538 (1992)
Pierazzo, E., Vickery, A. M. & Melosh, H. J. A reevaluation of impact melt production. Icarus 127, 408–423 (1997)
Ivanov, B. A. & Deutsch, A. in Large Impacts and Planetary Evolution (eds Dressler, B. O. & Sharpton, V. L.) 389–396 (Geological Society of America, Special Paper Vol. 339, 1999)
Therriault, A. M., Fowler, A. D. & Grieve, R. A. F. The Sudbury Igneous Complex: a differentiated impact melt-sheet. Econ. Geol. 97, 1521–1540 (2002)
Ames, D. E., Golightly, J. P., Lightfoot, P. C. & Gibson, H. L. Vitric compositions in the Onaping Formation and their relationship to the Sudbury Igneous Complex, Sudbury Structure. Econ. Geol. 97, 1541–1562 (2002)
Ames, D. E., Watkinson, D. H. & Parrish, R. R. Dating of a regional hydrothermal system induced by the 180 Ma Sudbury impact event. Geology 26, 447–450 (1998)
Coleman, A. P. The Sudbury nickel deposits. Ontario Bureau Mines Rep. 1902, 253–303 (1903)
Lightfoot, P. C., Keays, R. R., Morrison, G. G., Bite, A. & Farrell, K. P. Geochemical relationships in the Sudbury Igneous Complex: origin of the main mass and Offset dikes. Econ. Geol. 92, 289–307 (1997)
Cowan, E. J. & Schwerdtner, W. M. in Proceedings of the Sudbury-Noril'sk Symposium (eds Lightfoot, P. C. & Naldrett, A. J.) 45–56 (Ontario Geological Survey, Special Vol. 5, 1994)
Richardson, T. & Burnham, O. M. Precious metal analysis at the Geoscience Laboratories: results from the new low-level analytical facility. Ont. Geol. Surv. Open File Rep. 6100, 35 (2002)
Dickin, A. P., Nguyen, T. & Crockett, J. H. in Large Impacts and Planetary Evolution (eds Dressler, B. O. & Sharpton, V. L.) 361–371 (Geological Society of America, Special Paper Vol. 339, 1999)
Mungall, J. E. Program with Abstracts for 38th Annual GSA Northeastern Division Meeting, Halifax 23–29 (Geological Society of America, 2003)
Lightfoot, P. C. & Farrow, C. E. G. Geology, geochemistry, and mineralogy of the Worthington Offset dike: a genetic model for Offset dike mineralization in the Sudbury Igneous Complex. Econ. Geol. 97, 1419–1446 (2002)
Wedepohl, K. H. The composition of the continental crust. Geochim. Cosmochim. Acta 59, 1217–1232 (1995)
Gao, S. et al. Chemical composition of the continental crust as revealed by studies in East China. Geochim. Cosmochim. Acta 62, 1959–1975 (1998)
Pope, K. O., Kieffer, S. W. & Ames, D. E. Empirical and theoretical comparisons of the Chicxulub and Sudbury Impact Craters. Meteorit. Planet. Sci. 39, 97–116 (2004)
Campins, H. & Swindle, T. D. Expected characteristics of cometary meteorites. Meteorit. Planet. Sci. 33, 1201–1211 (1998)
McDonough, W. F. & Sun, S.-s. The composition of the Earth. Chem. Geol. 120, 223–253 (1995)
Paťava, J., Barnes, S.-J. & Vymazalová, A. The use of mantle normalization and metal ratios in the identification of the sources of platinum-group elements in various metal-rich black shales. Mineral. Dep. 38, 775–783 (2003)
Alvarez, L. W., Alvarez, W., Asaro, F. & Michel, H. V. Extraterrestrial cause for the Cretaceous-Tertiary boundary extinction. Science 208, 1095–1108 (1980)
Colodner, D. C., Boyle, E. A., Edmond, J. M. & Thomson, J. Post-depositional mobility of platinum, iridium and rhenium in marine sediments. Nature 358, 402–404 (1992)
Heymann, D. et al. in Large Impacts and Planetary Evolution (eds Dressler, B. O. & Sharpton, V. L.) 345–360 (Geological Society of America, Special Paper Vol. 339, 1999)
Acknowledgements
This study was generously supported by the University of Toronto, by the Geoscience Laboratories of the Ontario Geological Survey, and by the Geological Survey of Canada.Author's contributions Mapping and sampling was performed by J.E.M., D.E.A. and J.J.H.; geochemical interpretation was done by J.E.M., D.E.A. and J.J.H., in decreasing order of relative contribution.
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Mungall, J., Ames, D. & Hanley, J. Geochemical evidence from the Sudbury structure for crustal redistribution by large bolide impacts. Nature 429, 546–548 (2004). https://doi.org/10.1038/nature02577
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DOI: https://doi.org/10.1038/nature02577
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