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2017 | 8 | 100-109
Article title

Fragmenty kopalnego meteorytu z Lechówki: charakterystyka mineralogiczna i geochemiczna

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EN
Fragments of strongly weathered meteorite from Lechówka: mineralogical and geochemical characterisation
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PL
Abstracts
EN
Fossil iron meteorites are extremely rare in the geological sedimentary record. In the boundary clay from the outcrop at the Lechówka quarry (Poland), fragments of the paleometeorite were found in the Cretaceous-Paleogene boundary clay layer. The fragments of meteorite (2–6 mm in size) and meteoritic dust are metallic-grey in colour. Analyses of the meteorite from Lechówka reveal the presence of Ni-rich minerals with a total Ni amount of 2–3 wt%. They are represented by: taenite, kamacite, schreibersite, Ni-rich magnetite, and Ni-rich goethite. The investigated remnants of paleometeorite apparently represent an independent fall and does not seem to be derived from the K-Pg impactor.
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Year
Volume
8
Pages
100-109
Physical description
References
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Document Type
article
Publication order reference
YADDA identifier
bwmeta1.element.psjd-240af459-3f6c-4d9d-9fad-84e668aafa61
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