Abstract
The paper presents results of detailed magnetomineralogical and microprobe studies of sediments at the Cretaceous/Paleogene (K/T) boundary in two epicontinental sections in the Eastern Alps (Austria), where deposits, including the K/T boundary, outcrop along the Gams River and its tributaries. K/T boundary layers in these sections are similar in the set of such magnetic minerals as iron hydroxides, ferrospinels, hemoilmenite, titanomagnetite, magnetite, hematite, and metallic iron. However, the boundary layer in the Gams-1 section is distinguished by the presence of metallic nickel and its alloy with iron and by the absence of iron sulfides, whereas nickel has not been discovered in the Gams-2 section, which, however, contains iron sulfides of the pyrite type. Therefore, these minerals occur locally. It is suggested that enrichment in iron hydroxides of a common origin can be regarded as a global phenomenon inherent in the K/T boundary and unrelated to an impact event.
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Original Russian Text © A.F. Grachev, D.M. Pechersky, S.E. Borisovskii, V.A. Tselmovich, 2008, published in Fizika Zemli, 2008, No. 10, pp. 40–55.
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Grachev, A.F., Pechersky, D.M., Borisovskii, S.E. et al. Magnetic minerals in sediments at the Cretaceous/Paleogene boundary (the Gams Section, Eastern Alps). Izv., Phys. Solid Earth 44, 789–803 (2008). https://doi.org/10.1134/S1069351308100078
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DOI: https://doi.org/10.1134/S1069351308100078