Abstract:
:The research investigated three iron carbonate (siderite) sedimentary concretions from Nagykovácsi, Úri and Délegyháza, Hungary. To identify possible source rocks and effects of the glaze-like exposed surface of the concretions, we carried on comparative petrological, mineralogical, geochemical and isotopic studies. The samples were microbially mediated siderite concretions with embedded metamorphous and igneous mineral clasts, and had specific rim belts characterized by semi-concentric outer Fe-oxide layers, fluffy pyrite-rich outer belts and siderite inner parts. We investigated the cross section of the Fe-carbonate concretions by independent methodologies in order to identify their rim effects. Their surficial oxide layers showed evidence of degassing of the exposed surface caused most probably by elevated temperatures. The inner rim pyrite belt in the concretions excluded the possibility of a prolonged wet surface environment. Microtextural and mineralogical features did not support desert varnish formation. 10Be nuclide values of the Nagykovácsi and Uri concretions were far above the level of terrestrial in-situ cosmogenic nuclides, but they were consistent with the lowest levels for meteorites. Though the data were not conclusive to confirm any kind of known origin, they are contradictary, and open possibilities for a scenario of terrestrial meteorite origin.
journal_name
J Environ Radioactjournal_title
Journal of environmental radioactivityauthors
Polgári M,Bérczi S,Horiuchi K,Matsuzaki H,Kovács T,Józsa S,Bendő Z,Fintor K,Fekete J,Homonnay Z,Kuzmann E,Gucsik A,Gyollai I,Kovács J,Dódony Idoi
10.1016/j.jenvrad.2016.11.005subject
Has Abstractpub_date
2017-07-01 00:00:00pages
58-69eissn
0265-931Xissn
1879-1700pii
S0265-931X(16)30554-9journal_volume
173pub_type
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