Small Scale Heterogeneities in K/T Boundary Tektites From Mimbral

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Chicxulub, Cretaceous-Tertiary Boundary, Heterogeneity, Proximal Ejecta, Tektites

Scientific paper

Relict tektites from El Mimbral, Mexico are from K/T boundary deposits considered to be proximal ejecta related to the Chicxulub impact crater on the Yucatan peninsula. Our dark-brown Mimbral clasts are from the spherule bed (layer 1 of Bohor & Betterton) just above the latest Maastrichtian Mendez formation and are postulated to have been deposited initially in a shallow water environment. Relict tektites examined in this study are similar in bulk composition to those in previous reports of Mimbral tektites. Previous studies describe compositions determined to be homogenous on the 10-100 micron scale. However, spot analyses of Mimbral glass reveal small scale heterogeneities within individual fragments which were not optically apparent. Elemental mapping was utilized to illuminate heterogeneities in the range of 5 to 100 microns and to more clearly characterize their distribution. Compositional variations determined by mapping have been quantified by spot analysis and are described here.

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