Chemical relationships among irghizites, zhamanshinites, Australasian tektites and Henbury impact glasses

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Geochemistry, Glass, Petrology, Tektites, Australites, Chemical Evolution, Rare Earth Elements, Refractory Materials, Trace Elements, Chemistry, Irghizites, Zhamanshinites, Data, Impact Glasses, Analysis, Elements, Silica, Composition, Ages, Samples, Terrestrial, Tektites, Isotopic Composition, Craters, Electron Probes, Spectrometry, Spectroscopy, Spectrophotometry, Geochemistry, Nickel, Cobalt, Trace Elements, Chalcophile Elements, Rare Earth Elements

Scientific paper

Analytical data for elements in irghizites and zhamanshinites from the Zhamanshin impact structure, Kazakstan, USSR, Australasian tektites, Henbury impact glass, and parental Henbury subgreywacke sedimentary rocks are presented. Sample selection, analytical methods, geochemical comparisons, major constituents such as SiO2, MgO, and CaO, nickel and cobalt contents, volatile and chalcophile elements, refractory trace elements, rare earth elements, the relationship between irghizites and zhamanshinites, and the relationship between irghizites and tektites are discussed. It is concluded that the close similarity in chemistry and age between the silica-rich samples from Zhamanshin and Javan tektites from the Australasian strewnfield warrants a close examination of the Zhamanshin impact structure as a possible source for the Australasian tektites.

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