Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust

dc.contributor.authorFedorowicz, Stanisław
dc.contributor.authorStankowski, Wojciech T.J.
dc.date.accessioned2016-12-13T13:07:25Z
dc.date.available2016-12-13T13:07:25Z
dc.date.issued2016-12
dc.description.abstractThe date of fall of the Morasko iron meteorite was determined by means of thermoluminescence measurements of the fusion crust and related local materials. Three small pieces, commonly referred to as ‘shrapnel’, were used. The results obtained are 4.5–5.0 ka, which is in good agreement with previous estimates of 4–6 ka on the basis of radiometric, do- simetric and palynological methods.pl_PL
dc.identifier.citationGeologos, 2016, 22, 3, pp. 251-258pl_PL
dc.identifier.isbnISBN 978-83-232187-4-6
dc.identifier.issnISSN 1426-8981
dc.identifier.urihttp://hdl.handle.net/10593/16467
dc.language.isoengpl_PL
dc.publisherInstytut Geologii UAMpl_PL
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjectiron meteoritepl_PL
dc.subjectterrestrial agepl_PL
dc.subjectdosimetrypl_PL
dc.subjectPolandpl_PL
dc.titleDating the Morasko meteorite fall by natural thermoluminescence of the fusion crustpl_PL
dc.typeArtykułpl_PL

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Uniwersytet im. Adama Mickiewicza w Poznaniu
Biblioteka Uniwersytetu im. Adama Mickiewicza w Poznaniu
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