The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico

The Chicxulub impact crater is part of a select group of unique geological sites, being a natural laboratory to investigate crater formation processes and global effects of large-scale impacts. Chicxulub is one of only three multi-ring craters documented in the terrestrial record and impact has been related to the global environmental/climatic effects and mass extinction that mark the Cretaceous/Paleogene (K/Pg) boundary. The crater is buried under ~1.0 km of carbonate sediments in the Yucatan peninsula. The buried structure was initially identified from geophysical surveys of the PEMEX oil exploration program in southeastern Mexico. On the surface its influence is marked by the circular ring of cenotes that have formed from differential compaction and fracturing between the impact breccias and surrounding limestone sequences. The crater is about ~200 km in rim diameter, half on-land and half off-shore with geometric center at Chicxulub Puerto, making it possible to use land, marine and aerial geophysical methods. The Yucatan carbonate platform is an ideal place to have the crater, tectonically stable with no volcanic activity, having formed by slow deposition of carbonate sediments. These characteristics permit high resolution imagery of the crater underground structure with unprecedented detail. The impact and crater formation occur instantaneously, with excavation of the crust down to ~25 km depths in fractions of a second and lower crust uplift and crater formation in the next few hundred seconds. Energy release results in intense fracturing and deformation at the target site, generating seismic waves traveling the whole Earth. Understanding the physics of impacts on planetary surfaces and modeling of crustal deformation and rheological behavior of materials at high temperatures and pressures remain major challenges in geosciences. The K/Pg ejecta layer is the only global stratigraphic marker in the geological record, allowing correlation of events worldwide. In the last 20 years much has been learned about the Chicxulub crater and the K/Pg boundary; however what is perhaps most interesting are the questions remaining, which include fundamental aspects of Chicxulub impact and its environmental effects.

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Main Authors: Urrutia-Fucugauchi,Jaime, Camargo-Zanoguera,Antonio, Pérez-Cruz,Ligia, Pérez-Cruz,Guillermo
Format: Digital revista
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2011
Online Access:http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0016-71692011000100009
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spelling oai:scielo:S0016-716920110001000092011-10-05The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of MexicoUrrutia-Fucugauchi,JaimeCamargo-Zanoguera,AntonioPérez-Cruz,LigiaPérez-Cruz,Guillermo Chicxulub crater Cretaceous/Paleogene boundary cratering geophysical exploration methods drilling Yucatan platform Gulf of Mexico The Chicxulub impact crater is part of a select group of unique geological sites, being a natural laboratory to investigate crater formation processes and global effects of large-scale impacts. Chicxulub is one of only three multi-ring craters documented in the terrestrial record and impact has been related to the global environmental/climatic effects and mass extinction that mark the Cretaceous/Paleogene (K/Pg) boundary. The crater is buried under ~1.0 km of carbonate sediments in the Yucatan peninsula. The buried structure was initially identified from geophysical surveys of the PEMEX oil exploration program in southeastern Mexico. On the surface its influence is marked by the circular ring of cenotes that have formed from differential compaction and fracturing between the impact breccias and surrounding limestone sequences. The crater is about ~200 km in rim diameter, half on-land and half off-shore with geometric center at Chicxulub Puerto, making it possible to use land, marine and aerial geophysical methods. The Yucatan carbonate platform is an ideal place to have the crater, tectonically stable with no volcanic activity, having formed by slow deposition of carbonate sediments. These characteristics permit high resolution imagery of the crater underground structure with unprecedented detail. The impact and crater formation occur instantaneously, with excavation of the crust down to ~25 km depths in fractions of a second and lower crust uplift and crater formation in the next few hundred seconds. Energy release results in intense fracturing and deformation at the target site, generating seismic waves traveling the whole Earth. Understanding the physics of impacts on planetary surfaces and modeling of crustal deformation and rheological behavior of materials at high temperatures and pressures remain major challenges in geosciences. The K/Pg ejecta layer is the only global stratigraphic marker in the geological record, allowing correlation of events worldwide. In the last 20 years much has been learned about the Chicxulub crater and the K/Pg boundary; however what is perhaps most interesting are the questions remaining, which include fundamental aspects of Chicxulub impact and its environmental effects.info:eu-repo/semantics/openAccessUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica internacional v.50 n.1 20112011-03-01info:eu-repo/semantics/articletext/htmlhttp://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0016-71692011000100009en
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country México
countrycode MX
component Revista
access En linea
databasecode rev-scielo-mx
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region America del Norte
libraryname SciELO
language English
format Digital
author Urrutia-Fucugauchi,Jaime
Camargo-Zanoguera,Antonio
Pérez-Cruz,Ligia
Pérez-Cruz,Guillermo
spellingShingle Urrutia-Fucugauchi,Jaime
Camargo-Zanoguera,Antonio
Pérez-Cruz,Ligia
Pérez-Cruz,Guillermo
The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
author_facet Urrutia-Fucugauchi,Jaime
Camargo-Zanoguera,Antonio
Pérez-Cruz,Ligia
Pérez-Cruz,Guillermo
author_sort Urrutia-Fucugauchi,Jaime
title The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
title_short The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
title_full The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
title_fullStr The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
title_full_unstemmed The Chicxulub multi-ring impact crater, Yucatan carbonate platform, Gulf of Mexico
title_sort chicxulub multi-ring impact crater, yucatan carbonate platform, gulf of mexico
description The Chicxulub impact crater is part of a select group of unique geological sites, being a natural laboratory to investigate crater formation processes and global effects of large-scale impacts. Chicxulub is one of only three multi-ring craters documented in the terrestrial record and impact has been related to the global environmental/climatic effects and mass extinction that mark the Cretaceous/Paleogene (K/Pg) boundary. The crater is buried under ~1.0 km of carbonate sediments in the Yucatan peninsula. The buried structure was initially identified from geophysical surveys of the PEMEX oil exploration program in southeastern Mexico. On the surface its influence is marked by the circular ring of cenotes that have formed from differential compaction and fracturing between the impact breccias and surrounding limestone sequences. The crater is about ~200 km in rim diameter, half on-land and half off-shore with geometric center at Chicxulub Puerto, making it possible to use land, marine and aerial geophysical methods. The Yucatan carbonate platform is an ideal place to have the crater, tectonically stable with no volcanic activity, having formed by slow deposition of carbonate sediments. These characteristics permit high resolution imagery of the crater underground structure with unprecedented detail. The impact and crater formation occur instantaneously, with excavation of the crust down to ~25 km depths in fractions of a second and lower crust uplift and crater formation in the next few hundred seconds. Energy release results in intense fracturing and deformation at the target site, generating seismic waves traveling the whole Earth. Understanding the physics of impacts on planetary surfaces and modeling of crustal deformation and rheological behavior of materials at high temperatures and pressures remain major challenges in geosciences. The K/Pg ejecta layer is the only global stratigraphic marker in the geological record, allowing correlation of events worldwide. In the last 20 years much has been learned about the Chicxulub crater and the K/Pg boundary; however what is perhaps most interesting are the questions remaining, which include fundamental aspects of Chicxulub impact and its environmental effects.
publisher Universidad Nacional Autónoma de México, Instituto de Geofísica
publishDate 2011
url http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0016-71692011000100009
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