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Impact lithologies and their emplacement in the Chicxulub impact crater: Initial results from the Chicxulub Scientific Drilling Project, Yaxcopoil, Mexico
Abstract
Abstract— The Chicxulub Scientific Drilling Project (CSDP), Mexico, produced a continuous core of material from depths of 404 to 1511 m in the Yaxcopoil‐1 (Yax‐1) borehole, revealing (top to bottom) Tertiary marine sediments, polymict breccias, an impact melt unit, and one or more blocks of Cretaceous target sediments that are crosscut with impact‐generated dikes, in a region that lies between the peak ring and final crater rim. The impact melt and breccias in the Yax‐1 borehole are 100 m thick, which is approximately 1/5 the thickness of breccias and melts exposed in the Yucatán‐6 exploration hole, which is also thought to be located between the peak ring and final rim of the Chicxulub crater. The sequence and composition of impact melts and breccias are grossly similar to those in the Yucatán‐6 hole. Compared to breccias in other impact craters, the Chicxulub breccias are incredibly rich in silicate melt fragments (up to 84% versus 30 to 50%, for example, in the Ries). The melt in the Yax‐1 hole was produced largely from the silicate basement lithologies that lie beneath a 3 km‐ thick carbonate platform in the target area. Small amounts of immiscible molten carbonate were ejected with the silicate melt, and clastic carbonate often forms the matrix of the polymict breccias. The melt unit appears to have been deposited while molten but brecciated after solidification. The melt fragments in the polymict breccias appear to have solidified in flight, before deposition, and fractured during transport and deposition.
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“At Chicxulub, drill holes C-1 and S-1 indicate impactmelt-bearing lithologies (suevitic breccia and impact-melt rock) of unknown thickness (>500 m) interior to the inner topographic ring (e.g., Kring et al. 2004), which is consistent with the occurrence of the SIC interior to the postulated position of the inner topographic ring at Sudbury.”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Kring et al. 2004
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Research works printed but not linked: 78
- 10.1007/BF00371219 · DOI
- ArtemievaN. A. StöfflerD. HechtL. SchmittR. T. andTagleR.2003.Interaction of the ejecta plume and the atmosphere during the deposition of the uppermost suevite layers at the Yax‐1 drilling site Chicxulub Mexico(abstract #4063). 3rd International Conference on Large Meteorite Impacts. CD‐ROM.
- Bateson J. H., 1977, The geology of the Maya Mountains, Belize. Overseas Memoir 3, 43
- 10.1111/j.1945-5100.2004.tb01130.x · DOI · Paper page
- 10.1126/science.257.5073.1104 · DOI
- 10.1038/364325a0 · DOI
- Camargo‐Zanoguera A., 1994, Evidencia sismica del crater de impacto de Chicxulub, Boletín de la Asociación Mexicana de Geofísicos de Exploración, 34, 1
- 10.1190/1.1437578 · DOI
- 10.1111/j.1945-5100.2003.tb00315.x · DOI
- 10.1006/icar.2002.6822 · DOI · Paper page
- Cornejo Toledo A., 1950, Las anomalias gravimetricas en la cuenca salina del istmo, planicie costera de Tabasco, Campeche y Peninsula de Yucatán, Boletín de la Asociación Mexicana de Geólogos Petroleros, 2, 453
- Delgado‐Rodríguez O., 2001, Occam and Bostick 1‐D inversion of magnetotelluric soundings in the Chicxulub impact crater, Yucatán, Mexico, Geofísica Internacional, 40, 271, 10.22201/igeof.00167169p.2001.40.4.410 · DOI
- Donnelly T. W., 1990, The Geology of North America, Vol. H—The Caribbean Region, 37
- 10.1029/2003EO140001 · DOI
- DresslerB. O. SharptonV. L. andMarinL. E.2003b.Chicxulub Yax‐1 impact breccias: Whence they come? (abstract #1259). 34th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1007/BF00404198 · DOI
- Gault D. E., 1968, Shock metamorphism of natural materials, 87
- 10.1126/science.162.3849.121 · DOI
- 10.1111/j.1945-5100.1999.tb01351.x · DOI
- Guzmán E. J., 1952, Developments in Mexico in 1952, Bulletin of the American Association of Petroleum Geologists, 37, 1506
- Hecht L., 2003, Petrography, composition, shock metamorphism, and geology of the impact formations of the ICDP drill core Yax‐1, Chicxulub crater, Mexico (abstract), Meteoritics & Planetary Science, 38, A97
- HildebrandA. R.andStansberryJ. A.1992.K/T boundary ejecta distribution predicts size and location of Chicxulub crater(abstract). 23rd Lunar and Planetary Science Conference. pp.537–538.
- 10.1130/0091-7613(1991)019<0867:CCAPCT>2.3.CO;2 · DOI · Paper page
- HildebrandA. R. PilkingtonM. GrieveR. A. F. RobertsonP. B. andPenfieldG. T.1992.Recent studies of the Chicxulub crater Mexico(abstract). 23rd Lunar and Planetary Science Conference. pp.539–540.
- 10.1038/376415a0 · DOI
- 10.1007/BF01128707 · DOI
- Hörz R., 1977, Impact and explosion cratering, 425
- 10.1029/RG021i008p01667 · DOI
- KenkmannT. WittmannA. ScherlerD. andSchmittR. T.2003a.Deformation features of the Cretaceous units of the ICDP‐Chicxulub drill core Yax‐1(abstract #1368). 34th Lunar and Planetary Science Conference. CD‐ROM.
- KenkmannT. WittmannA. ScherlerD. andStöfflerD.2003b.The Cretaceous sequence of the Chicxulub Yax‐1 drillcore: What is impact derived? (abstract #4075). 34th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1111/j.1945-5100.2000.tb01511.x · DOI
- 10.1029/95JE01768 · DOI
- 10.1016/0016-7037(91)90143-S · DOI
- 10.1038/358141a0 · DOI
- Kring D. A., 2002, Trajectories and distribution of material ejected from the Chicxulub impact crater: Implications for postimpact wildfires, Journal of Geophysical Research, 107
- KringD. A. HildebrandA. R. andBoyntonW. V.1991.The petrology of an andesitic melt rock and a polymict breccia from the interior of the Chicxulub structure Yucatán Mexico(abstract). 22nd Lunar and Planetary Science Conference. pp.755–756.
- 10.1016/0012-821X(94)90175-9 · DOI
- KringD. A. HörzF. andZurcherL.2003.Initial assessment of the excavation and deposition of impact lithologies exposed by the Chicxulub Scientific Drilling Project Yaxcopoil Mexico(abstract #1641). 34th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1007/978-1-4684-8535-6_7 · DOI
- Masaitis V. L., 1994, Large meteorite impacts and planetary evolution, 153
- Maxwell D. E., 1977, Impact and explosion cratering, 1003
- Melosh H. J., 1989, Impact cratering: A geologic process, 245
- 10.1130/0091-7613(1999)027<0407:CTTDOA>2.3.CO;2 · DOI · Paper page
- 10.1038/37291 · DOI · Paper page
- 10.1016/S0012-821X(00)00307-1 · DOI · Paper page
- 10.1029/RG013i002p00337 · DOI
- 10.1016/S0012-821X(01)00558-1 · DOI
- PenfieldG. T.andCamargo‐ZanogueraA.1981.Definition of a major igneous zone in the central Yucatán platform with aeromagnetics and gravity(abstract). Technical Program Abstracts and Biographies Society of Exploration Geophysicists 51st Annual International Meeting. pp.37.
- PenfieldG. T.andCamargo‐ZanogueraA.1991.Interpretation of geophysical cross sections on the north flank of the Chicxulub impact structure. Proceedings 22nd Lunar and Planetary Science Conference. pp.1051.
- 10.1016/S0012-821X(98)00263-5 · DOI
- 10.1029/98JE02496 · DOI
- Pilkington M., 1994, Gravity and magnetic field modeling and structure of the Chicxulub crater, Mexico, Journal of Geophysical Research, 99, 131470, 10.1029/94JE01089 · DOI · Paper page
- 10.1111/j.1945-5100.2004.tb00052.x · DOI · Paper page
- SchmittR. T. StöfflerD. andWittmannA.2003a.Shock metamorphism of impactite lithologies of the ICDP Chicxulub drill core Yax‐1(abstract #1327). 34th Lunar and Planetary Science Conference. CD‐ROM.
- SchmittR. T. WittmannA. andStöfflerD.2003b.The ICDP drill core Yaxcopoil‐1 Chicxulub impact crater Mexico: Shock metamorphism of the impactite units (794–894 m)(abstract #4061). 34th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1038/359819a0 · DOI
- 10.1126/science.261.5128.1564 · DOI · Paper page
- 10.1130/0-8137-2307-8.55 · DOI · Paper page
- SharptonV. L. CorriganC. M. MarinL. E. Urrutia‐FucugauchiJ. andVogelT. A.1999.Characterization of impact breccias from the Chicxulub impact basin: Implications for excavation and ejecta emplacement(abstract #1515). 30th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1038/349482a0 · DOI
- 10.1038/353839a0 · DOI
- 10.1029/1999JB900001 · DOI
- StöfflerD. HechtL. KenkmannT. SchmittR. T. andWittmanA.2003a.Properties classification and genetic interpretation of the allochthonous impact formations of the ICDP Chicxulub drill core Yax‐1(abstract #1553). 34th Lunar and Planetary Science Conference. CD‐ROM.
- Stöffler D., 2003, Characteristics of the multi‐ring impact basin of Chicxulub, Mexico, as derived from drill core data and numerical modeling (abstract), Meteoritics & Planetary Science, 38, A126
- StöfflerD. IvanovB. A. HechtL. KenkmannT. SchmittR. T. SalgeT. SchönianR. TagleR. WeselerS. andWittmanA.2003c.Origin and emplacement of the impact formations at Chicxulub Mexico with special emphasis on the Yax‐1 deep drilling(abstract #4092). 3rd International Conference on Large Meteorite Impacts. CD‐ROM.
- 10.1126/science.257.5072.954 · DOI · Paper page
- 10.2113/gsecongeo.97.7.1521 · DOI · Paper page
- TuchschererM. G. ReimoldW. U. GibsonR. L. andKoeberlC.2003.Petrographic observations and classification: Impactites from the Yaxcopoil‐1 borehole Chicxulub impact structure Yucatán peninsula Mexico(abstract #1310). 34th Lunar and Planetary Science Conference. CD‐ROM.
- 10.1029/96GL01566 · DOI
- VickeryA. M. KringD. A. andMeloshH. J.1992.Ejecta associated with large terrestrial impacts: Implications for the Chicxulub impact and K/T boundary stratigraphy(abstract). 23rd Lunar and Planetary Science Conference. pp.1473–1474.
- 10.1007/BF01824968 · DOI
- Engelhardt W., 1969, Petrologische Untersuchungen im Ries, Geologica Bavarica, 6, 229
- 10.1130/0091-7613(1995)023<0873:YNSSIA>2.3.CO;2 · DOI · Paper page
- 10.1111/j.1945-5100.2002.tb00844.x · DOI
- WittmannA. KenkmannT. SchmittR. T. andStöfflerD.2003a.Clastic polymict dikes in the “megablock” sequence of the ICDP‐Chicxulub drill core Yax‐1(abstract #1386). 34th Lunar and Planetary Science Conference. CD‐ROM.
- WittmannA. KenkmannT. SchmittR. T. HechtL. andStöfflerD.2003b.Impact melt rocks in the “Cretaceous megablock sequence” of drill core Yaxcopoil‐1 Chicxulub crater Yucatán Mexico(abstract #4125). 3rd International Conference on Large Meteorite Impacts. CD‐ROM.
- 10.1111/j.1945-5100.2004.tb01137.x · DOI
- Zurcher L., 2004, Stable isotope record of post‐impact fluid activity in the Chicxulub crater as exposed by the Yaxcopoil‐1 borehole, Mexico
Cited by
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
Metadata
- Authors
- Kring, D. A., Hörz, F., Zurcher, L., & Fucugauchi, J. U.
- Venue
- Meteoritics & Planetary Science
- Publisher
- Wiley
- Published
- 2004-06
- Volume
- 39
- Issue
- 6
- Pages
- 879-897
- ISSN
- 1086-9379
- 1945-5100
- Cited by
- 70
- References
- 0
- Language
- en
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