Mathematics – Logic
Scientific paper
Aug 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992sci...257..954s&link_type=abstract
Science (ISSN 0036-8075), vol. 257, no. 5072, Aug. 14, 1992, p. 954-958. Research supported by Institute of Human Origins, Petro
Mathematics
Logic
130
Breccia, Cretaceous-Tertiary Boundary, Impact Melts, Meteorite Craters, Radioactive Age Determination, Tektites, Geochemistry, Isotope Effect, Petrology
Scientific paper
Ar-40/Ar-39 dating of drill-core samples of a glassy melt rock recovered from beneath a massive impact breccia contained with the 180-kilometer subsurface Chicxulub crater yields well-behaved incremental heating spectra with a mean plateau age of 64.98 +/- 0.05 million years ago (Ma). The glassy melt rock of andesitic composition was obtained from core 9 (1390 to 1393 meters) in the Chicxulub 1 well. The age of the melt rock is virtually indistinguishable from Ar-40/Ar-39 ages obtained on tektite glass from Beloc, Haiti, and Arroyo el Mimbral, northeastern Mexico, of 65.01 +/- 0.08 Ma (mean plateau age for Beloc) and 65.07 +/- 0.10 Ma (mean total fusion age for both sites). The Ar-40/Ar-39 ages, in conjunction with geochemical and petrological similarities, strengthen the suggestion that the Chicxulub structure is the source for the Haitian and Mexican tektites and is a viable candidate for the Cretaceous-Tertiary boundary impact site.
Alvarez Walter
Cedillo-Pardo Esteban
Claeys Philippe
Curtis Garniss H.
Grajales-Nishimura José M.
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