Portal de Periódicos da CAPES

Chicxulub impact: The origin of reservoir and seal facies in the southeastern Mexico oil fields: Comment and Reply

2001; Geological Society of America; Volume: 29; Issue: 1 Linguagem: Inglês

10.1130/0091-7613(2001)029 2.0.co;2

1943-2682

Wolfgang Stinnesbeck, Gerta Keller, Thierry Adatte,

Astro and Planetary Science

Research Article| January 01, 2001 Chicxulub impact: The origin of reservoir and seal facies in the southeastern Mexico oil fields: Comment and Reply Wolfgang Stinnesbeck; Wolfgang Stinnesbeck 1Geologisches Institut, Universität Karlsruhe, Postfach 6980, 76128 Karlsruhe, Germany Search for other works by this author on: GSW Google Scholar Gerta Keller; Gerta Keller 2Department of Geosciences, Princeton University, Princeton, New Jersey 08544, USA Search for other works by this author on: GSW Google Scholar Thierry Adatte Thierry Adatte 3Institut de Géologie, Université de Neuchâtel, 11 rue Emile-Argand, 2007 Neuchâtel, Switzerland Search for other works by this author on: GSW Google Scholar Geology (2001) 29 (1): 94–95. https://doi.org/10.1130/0091-7613(2001)029 2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Wolfgang Stinnesbeck, Gerta Keller, Thierry Adatte; Chicxulub impact: The origin of reservoir and seal facies in the southeastern Mexico oil fields: Comment and Reply. Geology 2001;; 29 (1): 94–95. doi: https://doi.org/10.1130/0091-7613(2001)029 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Grajales-Nishimura et al. (2000) suggested that “offshore oil-producing breccias and seals from oil fields in the Campeche marine plateform are of K-T boundary age and that their mode of formation is probably related to the K-T impact event at Chicxulub.” The basis for this interpretation is the assumption that the siliciclastic deposits in Cretaceous-Tertiary (K-T) boundary sections in Texas, Alabama, and northeastern Mexico, and limestone breccia deposits in Cuba, the Campeche marine platform, and in southern Mexico (e.g., Guayal, Bochil) are impact ejecta-, megatsunami-, and debris flow deposits triggered by the Chicxulub impact. However, the stratigraphic ages of these deposits... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.