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Vredefort, Sudbury, Chicxulub: Three of a Kind?
Abstract
Vredefort, Sudbury, and Chicxulub are the largest known terrestrial impact structures. All have been cited as multi-ring basins. The available data indicate that all have some form of multiple-ring attributes, most commonly structural features. Chicxulub, however, is the only example with morphological ring features. There are also commonalities in the structural and lithological features of Vredefort and Sudbury, and it is possible to construct a generalized compilation of the character of 200–300 km diameter impact basins on Earth. It is not clear, however, that any of these structures had the original morphological characteristics of large lunar multi-ring basins. Additional data and synthesis are required to fully characterize these structures in order to realize their potential to constrain large-scale cratering processes. If this is not sufficient incentive for further studies (the environmental effects of Chicxulub aside), the Vredefort, Sudbury, and Chicxulub impact events are also the reason for the existence of world-class mineral and hydrocarbon deposits.
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“Previously, some degree of commonality between Vredefort, Sudbury, and Chicxulub had been noted, but how the various”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Grieve and Therriault 2000
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Research works printed but not linked: 148
- 10.1126/science.208.4448.1095 · DOI
- 10.1130/0091-7613(1998)026<0447:DOARHS>2.3.CO;2 · DOI
- Bishopp DW. 1941. The geodynamics of the Vredefort Dome.Trans. Geol. Soc. S. Afr.44: 1–18
- 10.1126/science.224.4651.867 · DOI
- 1937, Field Lab., 5, 53
- Brett R. 1992. The Cretaceous-Tertiary extinction: a lethal mechanism involving anhydrite target rocks.Geochim. Cosmochim. Acta56:3603–6 · DOI
- Brink MC, Waanders FB, Bisschoff AA. 1997. Vredefort: a model for the anatomy of an astrobleme.Tectonophysics270:83–114 · DOI · Paper page
- 1994, Geol. Soc. Am. Sp. Pap., 293, 319
- 1994, Bol. Ass. Mex. Geofis. Explor., 1
- Card KD. 1994. Geology of the Levack gneiss complex, the northern footwall of the Sudbury Structure, Ontario. InCurrent Research 1994-C,pp. 269–76. Geological Survey of Canada · DOI
- 10.2475/ajs.263.9.786 · DOI · Paper page
- Carter NL. 1968. Dynamic deformation of quartz. InShock Metamorphism of Natural Materials,ed. BM French, NM Short, pp. 453–74. Baltimore: Mono Book Corp. 644 pp.
- Carter NL, Officer CB, Chesner CA, Rose WI. 1986. Dynamic deformation of volcanic ejecta from Toba caldera: possible relevance to the Cretaceous/Tertiary boundary phenomena.Geology14:380–83 · DOI
- 10.1016/0009-2541(94)90068-X · DOI
- Christeson G, Nakamura Y, Buffler R, the Chicxulub Working Group. 1999. Upper crustal structure of the Chicxulub impact crater from wide-angle ocean bottom seismograph data. See Dressler & Sharpton 1999. In press · DOI
- 10.2113/gsecongeo.91.7.1263 · DOI
- Corner B, Reimold WU, Brandt D, Koeberl C. 1997. Morokweng impact structure, Northwest Province, South Africa: geophysical imaging and shock petrographic studies.Earth Planet. Sci.146:351–64 · DOI
- 1972, Geol. Assoc. Can. Sp. Pap., 10, 7
- Deutsch A, Grieve RAF, Avermann M, Bischoff L, Brockmeyer P, et al. 1995. The Sudbury Structure (Ontario, Canada): a tectonically deformed multi-ring basin.Geol. Rundsch.84:697–709 · DOI
- 10.1016/0016-7037(96)00044-0 · DOI
- 10.1016/0016-7037(92)90396-Z · DOI
- Dietz RS. 1961. Vredefort ring structure: meteorite impact scar?J. Geol.69:499–516 · DOI
- Dietz RS. 1962. Sudbury Structure as an astrobleme.Trans. Am. Geophys. Union43:445–46 (Abstr.)
- 10.1086/626999 · DOI
- Donofrio RR. 1997. Survey of hydrocarbon-producing impact structures in North America: exploration results to date and potential for discovery in Precambrian basement rocks. See Johnson & Campbell 1997, pp. 17–29
- Dressler BO. 1984. The effects of the Sudbury Event and the intrusion of the Sudbury Igneous Complex on the footwall rocks of the Sudbury Structure. See Pye et al 1984, pp. 97–136
- Dressler BO, Gupta VK, Muir TL. 1991. The Sudbury Structure. InGeology of Ontario,ed. P Thurston, H Williams, R Sutcliffe, G Stott, 1:593–625. Ontario Geological Survey Sp. Vol. 4. Toronto: Ministry of Northern Development and Mines. 1525 pp.
- 10.1016/0016-7037(96)00067-1 · DOI
- Faggart BE, Basu AR, Tatsumoto A. 1985. Origin of the Sudbury complex by meteorite impact: Neodymium isotopic evidence.Science230:436–39 · DOI
- French BM. 1967. Sudbury Structure, Ontario: some petrographic evidence for origin by meteorite impact.Science156:1094–98 · DOI
- French BM, Nielsen RL. 1990. Vredefort Bronzite Granophyre: chemical evidence for origin as a meteorite impact melt.Tectonophysics171:119–38 · DOI
- 10.1130/0016-7606(1997)109<0268:DOAMCO>2.3.CO;2 · DOI
- Ganapathy R. 1980. A major meteorite impact on Earth 65 million years ago: evidence from the Cretaceous-Tertiary boundary clay.Science209:921–23 · DOI
- Giblin PE. 1984. Glossary of Sudbury geology terms. See Pye et al 1984, pp. 571–74
- Gibson RL, Armstrong RA, Reimold WU. 1997a. The age and thermal evolution of the Vredefort impact structure: a single-grain U-Pb zircon study.Geochim. Cosmochim. Acta61:1531–40 · DOI
- Gibson RL, Reimold WU, Wallmach T. 1997b. Origin of pseudotachylite in the lower Witwatersrand Supergroup, Vredefort Dome (South Africa): constraints from metamorphic studies.Tectonophysics283:241–62 · DOI
- Grieve RAF. 1994. An impact model of the Sudbury Structure. InProceedings of the Sudbury-Noril’sk Symposium,ed. PC Lightfoot, AJ Naldrett, pp. 119–32. Ontario: Ministry of Northern Development and Mines Sp. Vol. 5. 423 pp.
- Grieve RAF. 1997. Terrestrial impact structures: basic characteristics and economic significance with emphasis on hydrocarbon production. See Johnson & Campbell 1997, pp. 3–16
- 10.1016/S0273-1177(97)00877-6 · DOI
- Grieve RAF, Coderre JM, Robertson PB, Alexopoulos JS. 1990. Microscopic planar deformation features in quartz of the Vredefort structure: anomalous but still suggestive of an impact origin.Tectonophysics171:185–200 · DOI
- Grieve RAF, Dence MR, Robertson PB. 1977. Cratering processes as interpreted from the occurrence of impact melts. See Roddy et al 1977, pp. 791–814
- 10.1111/j.1945-5100.1989.tb00948.x · DOI
- Grieve RAF, Langenhorst F, Stöffler D. 1996. Shock metamorphism of quartz in nature and experiment: II. Significance in geoscience.Meteorit. Planet. Sci.31:6–35 · DOI
- 10.1080/00206819409465452 · DOI
- Grieve RAF, Stöffler D, Deutsch A. 1991. The Sudbury Structure: controversial or misunderstood.J. Geophys. Res.96:22,753–64 · DOI · Paper page
- 10.1086/627158 · DOI
- 1961, Trans. Geol. Soc. S. Afr., 64, 147
- Hart RJ, Andreoli MAG, Tredoux M, Dewit MJ. 1990. Geochemistry across an exposed section of Archaean crust at Vredefort, South Africa: with implications for mid-crustal discontinuities.Chem. Geol.82:21–50 · DOI
- Hart RJ, Hargraves RB, Andreoli MAG, Tredoux M, Doucouré CM. 1995. Magnetic anomaly near the center of the Vredefort structure: implications for impact-related magnetic signatures.Geology23:277–80 · DOI · Paper page
- Hart RJ, Welke HJ, Nicolaysen LO. 1981. Geochronology of the deep profile through Archaean basement at Vredefort, with implications for early crustal evolution.J. Geophys. Res.86:10,663–80 · DOI
- Henkel H, Reimold WU. 1998. Integrated geophysical modelling of a giant, complex impact structure: anatomy of the Vredefort Structure, South Africa.Tectonophysics287:1–20 · DOI · Paper page
- 10.1126/science.248.4957.843 · DOI
- Hildebrand AR, Penfield GT, Kring DA, Pilkington M, Camargo AZ, et al. 1991. Chicxulub crater: a possible Cretaceous/Tertiary boundary impact crater on the Yucatan Peninsula, Mexico.Geology19:867–71 · DOI · Paper page
- 10.1038/376415a0 · DOI
- Hildebrand AR, Pilkington M, Ortiz-Aleman C, Chavez RE, Urrutia-Fucugauchi J, et al. 1998. Mapping Chicxulub crater with gravity and seismic reflection data. InMeteorites: Flux with Time and Impact Effects,ed. MM Grady, R Hutchison, G McCall, D Rothery, pp. 155–76. London: Geol. Soc. London Sp. Publ. 140. 278 pp. · DOI · Paper page
- 1999, Sci. Avenir, 628, 131
- Jaupart C, Tait S. 1995. Dynamics of differentiation in magma reservoirs.J. Geophys. Res.100:17,615–36 · DOI
- 10.1016/0012-821X(95)00236-6 · DOI
- Kamo SL, Reimold WU, Krogh TE, Colliston WP. 1996. A 2.023 Ga age for the Vredefort impact event and a first report of shock metamorphosed zircons in pseudotachylitic breccias and Granophyre.Earth Planet. Sci. Lett.144:369–87 · DOI · Paper page
- 1990, S. Afr. J. Geol., 93, 350
- 10.1016/S0040-1951(97)00181-9 · DOI
- Koeberl C, Reimold WU, Shirey SB. 1996. Re-Os isotope and geochemical study of the Vredefort Granophyre: clues to the origin of the Vredefort structure, South Africa.Geology24:913–16 · DOI · Paper page
- Kring DA. 1993. The Chicxulub impact event and possible causes of the K/T boundary extinctions. InProc. 1st Annual Symposium of Fossils of Arizona,ed. D Boaz, H Dorman, pp. 63–79. Mesa, Arizona: Southwest Museum and Paleontological Society
- Kring DA. 1995. The dimensions of the Chicxulub impact crater and impact melt sheet.J. Geophys. Res.100:16,979–86 · DOI
- 10.1038/358141a0 · DOI
- Krogh TE, Davis DW, Corfu F. 1984. Precise U-Pb zircon and baddeleyite ages for the Sudbury area. See Pye et al 1984, pp. 431–46
- 10.1016/0012-821X(93)90150-8 · DOI
- Krogh TE, Kamo SL, Bohor BF. 1996. Shock metamorphosed zircons with correlated U-Pb discordance and melt rocks with concordant protolith ages indicate an impact origin for the Sudbury Structure. Special AGU Publication, Geophys. Moho. 95:343–53 · DOI
- 10.1038/288651a0 · DOI
- Lambert P. 1981. Breccia dikes: geological constraints on the formation of complex craters. See Merrill & Schultz 1981, pp. 59–78
- 10.1016/0040-1951(94)90137-6 · DOI · Paper page
- Leroux H, Warme JE, Doukhan J-C. 1995. Shocked quartz in the Alamo breccia, Southern Nevada: evidence for a Devonian impact event.Geology23:1003–6 · DOI · Paper page
- Lilly PA. 1981. Shock metamorphism in the Vredefort collar: evidence for internal shock sources.J. Geophys. Res.86:10,689–700 · DOI
- Loper DE, McCartney K. 1988. Shocked quartz found at the K/T boundary: a possible endogeneous mechanism.EOS69:961, 971–72 · DOI
- 10.1038/272715a0 · DOI · Paper page
- 10.1016/0012-821X(91)90167-G · DOI
- 10.1111/j.1525-1314.1992.tb00102.x · DOI
- Masaitis VL, Shafranovsky GI, Grieve RAF, Langenhorst F, Peredery WV, et al. 1999. Impact diamonds in the suevitic breccias of the Black Onaping Formation, Sudbury Structure, Ontario, Canada. See Dressler & Sharpton 1999. In press · DOI
- 1996, Geol. Soc. Am. Sp. Pap., 302, 347
- Melosh HJ. 1989.Impact Cratering: A Geologic Process.New York: Oxford Univ. Press. 245 pp.
- 10.1146/annurev.earth.27.1.385 · DOI
- 10.1029/GL005i011p00985 · DOI
- Merrill RB, Schultz PH, ed. 1981.Multi-Ring Basins.New York: Pergamon Press. 295 pp.
- 10.1130/0091-7613(1992)020<0807:DGOTSS>2.3.CO;2 · DOI
- 10.1029/93GL03424 · DOI · Paper page
- 10.1016/S0009-2541(98)00136-3 · DOI
- Molnár F, Watkinson DH, Jones PC, Gatter I. 1997. Fluid inclusion evidence for hydrothermal enrichment of magmatic ores at the contact zone of the Ni-Cu-platinum group element 4b Deposit, Lindsley Mine, Sudbury, Canada.Econ. Geol.92:674–85 · DOI
- Morgan J, Warner M. 1999. Chicxulub: the third dimension of a multi-ring impact basin.Geology27:407–10 · DOI · Paper page
- 10.1038/37291 · DOI · Paper page
- 10.1130/0091-7613(1997)025<0007:DTSWAT>2.3.CO;2 · DOI
- 10.1016/0040-1951(92)90168-6 · DOI
- 1990, S. Afr. J. Geol., 93, 180
- Naldrett AJ. 1984. Summary, discussion, and synthesis. See Pye et al 1984, pp. 533–70 · DOI
- Naldrett AJ, Asif M, Schandl E, Searey T, Morrison GG, et al. 1999. Platinum-group elements in the Sudbury Ores: significance with respect to the origin of different ores zones and to the exploration for footwall orebodies.Econ. Geol.94:185–210 · DOI
- Nicolaysen LO. 1990. The Vredefort structure: an introduction and a guide to recent literature.Tectonophysics171:1–6 · DOI
- 10.1126/science.227.4691.1161 · DOI
- Ostermann M, Shärer U, Deutsch A. 1996. Impact melt dikes in the Sudbury multi-ring basin (Canada): implications from uranium-lead geochronology on the Foy Offset Dike.Meteorit. Planet. Sci.31:494–501 · DOI
- Peredery WV. 1991. Geology and ore deposits of the Sudbury Structure, Ontario (Field Trip 7).Geol. Surv. Can. Open File2162. 41 pp. · DOI
- Pierazzo E, Kring DA, Melosh HJ. 1998. Hydrocode simulation of the Chicxulub impact event and the production of climatically active gases.J. Geophys. Res.103:28,607–25 · DOI
- 10.1016/S0012-821X(99)00192-2 · DOI
- 10.1111/j.1945-5100.1985.tb00846.x · DOI
- Pilkington M, Hildebrand AR, Ortiz-Aleman C. 1994. Gravity and magnetic field modeling and structure of the Chicxulub structure, Mexico.J. Geophys. Res.99:13,147–62 · DOI · Paper page
- Pope KO, Baines KH, Ocampo AC, Ivanov BA. 1994. Impact winter and the Cretaceous/Tertiary extinctions: results of the Chicxulub asteroid impact model.Earth Planet. Sci. Lett.128:719–25 · DOI
- 10.1130/0091-7613(1996)024<0527:SEOTCC>2.3.CO;2 · DOI · Paper page
- Pretorius DA. 1991. The sources of Witwatersrand gold and uranium: a continued difference in opinion.Econ. Geol. Mon.8:139–63 · DOI
- Pye E, Naldrett A, Giblin P. 1984.The Geology and Ore Deposits of Sudbury.Ontario Geological Survey Sp. Vol. 1. Ontario Ministry of Natural Resources. 604 pp.
- 1990, S. Afr. J. Geol., 93, 645
- 1993, J. Geol. Edu., 41, 106
- Reimold WU, Colliston WP. 1994. Pseudotachylites of the Vredefort Dome and the surrounding Witwatersrand Basin, South Africa. InLarge Meteorite Impacts and Planetary Evolution,ed. BO Dressler, RAF Grieve, VL Sharpton, pp. 177–96. Boulder, Colorado: Geol. Soc. Amer. Spec. Pap. 293. 348 pp. · DOI
- 10.1016/S0899-5362(96)00059-0 · DOI
- Reimold WU, Horsch H, Durrheim RJ. 1990. The “Bronzite” Granophyre from the Vredefort Structure—a detailed analytical study and reflections on the genesis of one of Vredefort’s enigmas.Proc. Lunar Planet. Sci. Conf.20th. pp. 433–50
- 1991, S. Afr. J. Sci., 87, 412
- Robertson PB, Grieve RAF. 1977. Shock attenuation at terrestrial impact structures. See Roddy et al 1977, pp. 687–702
- Roddy DJ, Pepin RO, Merrill RB, eds. 1977.Impact and Explosion Cratering.Oxford: Pergamon. 1301 pp.
- Roest WR, Pilkington M. 1994. Restoring post-impact deformation at Sudbury: a circular argument.Geophys. Res. Lett.21:959–62 · DOI
- 1997, Explor. Min. Geol., 6, 1
- Rousell DH, Long DGF. 1998. Are outliers of the Huronian Supergroup preserved in structures associated with collapse of the Sudbury impact crater?J. Geol.106:407–19 · DOI
- Santiago J, Baro A. 1990. Mexico’s giant fields, 1978–1988 decade. InGiant Oil and Gas Fields of the Decade 1978–1988,ed. M Halbouty, pp. 73–99. Tulsa, Oklahoma: Am. Assoc. Petrol. Geol.
- 10.1130/0091-7613(1996)024<0963:CTCIAA>2.3.CO;2 · DOI · Paper page
- 10.1126/science.271.5255.1573 · DOI
- 10.1016/S0040-1951(99)00124-9 · DOI
- 1916, Q. J. Geol. Soc. Lond., 62, 198
- Sharpton VL, Burke K, Camargo-Zanoguera A, Hall SA, Lee DS, et al. 1993. Chicxulub multiring impact basin: size and other characteristics derived from gravity analysis.Science261:1564–67 · DOI · Paper page
- 10.1038/359819a0 · DOI
- 1996, Geol. Soc. Am. Sp. Pap., 307, 55
- 1978, Trans. Geol. Soc. S. Afr., 81, 115
- Simpson C. 1981. Occurrence and orientation of shatter cones in Pretoria Group quartzites in the collar of the Vredefort Dome: impact origin precluded.J. Geophys. Res.86:10,701–6 · DOI
- 10.1038/287158a0 · DOI
- Snyder DB, Hobbs RW, the Chicxulub Working Group. 1999. Ringed structural zones with deep roots formed by the Chicxulub impact.J. Geophys. Res.104:10,743–55 · DOI
- 10.1130/0091-7613(1997)025<0627:ITAYHR>2.3.CO;2 · DOI
- 10.1111/j.1945-5100.1995.tb01132.x · DOI
- 10.1038/373130a0 · DOI · Paper page
- Spudis PD. 1993.The Geology of Multi-Ring Impact Basins.New York: Cambridge Univ. Press. 263 pp. · DOI
- Stöffler D, Langenhorst F. 1994. Shock metamorphism of quartz in nature and experiment: I. Basic observation and theory.Meteoritics29:155–81 · DOI
- Swisher CC, Grajales-Nishimura JM, Montanari A, Margolis SV, Claeys P, et al. 1992. Coeval40Ar/39Ar ages of 65.0 million years ago from Chicxulub Crater melt rock and Cretaceous-Tertiary boundary tektites.Science257:954–58 · DOI · Paper page
- Therriault AM, Grieve RAF, Reimold WU. 1997a. Original size of the Vredefort Structure: implications for the geological evolution of the Witwatersrand Basin.Meteorit. Planet. Sci.32:71–77 · DOI · Paper page
- 1997, S. Afr. J. Geol., 100, 115
- Thompson LM, Spray JG. 1996. Pseudotachylyte petrogenesis: constraints from the Sudbury impact structure.Contrib. Min. Pet.125:359–74 · DOI
- Thompson LM, Spray JG, Kelley SP. 1998. Laser probe argon-40/argon-39 dating of pseudo-tachylyte from the Sudbury Structure: evidence for postimpact thermal overprinting in the North Range.Meteorit. Planet. Sci.33:1259–69 · DOI · Paper page
- 10.1111/j.1945-5100.1998.tb01652.x · DOI · Paper page
- 10.1016/0040-1951(94)90161-9 · DOI
- Walker RJ, Morgan JW, Naldrett AJ, Li C, Fassett JD. 1991. Re-Os isotope systematics of Ni-Cu sulfide ores, Sudbury Igneous Complex, Ontario: evidence for a major crustal component.Earth Planet. Sci. Lett.105:416–29 · DOI
- 10.1016/0040-1951(90)90088-P · DOI
- Warme JE, Kuehner H-C. 1998. Anatomy of an anomaly: the Devonian catastrophic Alamo impact breccia of Southern Nevada.Intern. Geol. Rev.40:189–216 · DOI
- White JC. 1993. Shock-induced melting and silica polymorph formation, Vredefort Structure, South Africa. InDefects and Processes in the Solid State: Geoscience Applications,ed. JN Boland, JD Fitz Gerald, pp. 69–84. Holland: Elsevier. 470 pp.
- Wood CA, Head JW. 1976. Comparison of impact basins on Mercury, Mars and the Moon.Proc. Lunar Sci. Conf.7th. pp. 3629–51
- Wood CR, Spray JG. 1998. Origin and emplacement of Offset Dikes in the Sudbury impact structure: constraints from Hess.Meteorit. Planet. Sci.33:337–47 · DOI · Paper page
- 10.1029/94JB02647 · DOI
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Sorted by citations
GRIEVE, R. A. F., REIMOLD, W. U., MORGAN, J., RILLER, U., & PILKINGTON, M. (2008) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2008.tb01086.x · Cited by 90
Self-citationThe Sudbury impact layer in the Paleoproterozoic iron ranges of northern Michigan, USA
Cannon, W. F., Schulz, K. J., Horton, J. W., & Kring, D. A. (2010) · Geological Society of America Bulletin · doi:10.1130/b26517.1 · Cited by 68
Metadata
- Authors
- Grieve, R., & Therriault, A.
- Affiliations
- Earth Sciences Sector, Natural Resources Canada, Ottawa, Ontario K1A 0E8, Canada;
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 2000-05
- Volume
- 28
- Issue
- 1
- Pages
- 305-338
- ISSN
- 0084-6597
- 1545-4495
- Cited by
- 133
- References
- 0
- Language
- en
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