Ar-40 - Ar-39 dating of the Manson impact structure - A Cretaceous-Tertiary boundary crater candidate

Physics

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Argon Isotopes, Bolides, Cretaceous-Tertiary Boundary, Meteorite Craters, Mineralogy, Geochemistry, Meteoritic Damage, Spectrum Analysis, Structural Properties (Geology)

Scientific paper

The mineralogy of shocked mineral and lithic grains in the Cretaceous-Tertiary (K-T) boundary claystone worldwide is most consistent with a bolide impact on a continent. Both the concentrations and sizes of these shocked grains are greatest in the western interior of North America. These data suggest that the Manson impact structure in north-central Iowa is a viable candidate for the K-T boundary impact event. Argon-40-argon-39 age spectrum dating of shocked microcline from the crystalline central uplift of the Manson impact structure indicates that there was severe argon-40 loss at 65.7 + or - 1.0 million years ago, an age that is indistinguishable from that of the K-T boundary, within the limits of analytical precision.

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