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

The 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...

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Main Authors: Fedorowicz Stanisław, Stankowski Wojciech T. J.
Format: Article
Language:English
Published: Sciendo 2016-09-01
Series:Geologos
Subjects:
Online Access:https://doi.org/10.1515/logos-2016-0024
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spelling doaj-14df4a14b56e43e78b28c49833239e672021-09-06T19:20:05ZengSciendoGeologos2080-65742016-09-0122325125810.1515/logos-2016-0024logos-2016-0024Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crustFedorowicz Stanisław0Stankowski Wojciech T. J.1University of Gdańsk, Institute of Geography, Department of Geomorphology and Quaternary Geology,ul. Bażyńskiego 4, 80-950 Gdańsk, PolandInstitute of Geology, Adam Mickiewicz University, ul. Maków Polnych 16, 61-606 Poznań, PolandThe 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.https://doi.org/10.1515/logos-2016-0024iron meteoriteterrestrial agedosimetrypoland
collection DOAJ
language English
format Article
sources DOAJ
author Fedorowicz Stanisław
Stankowski Wojciech T. J.
spellingShingle Fedorowicz Stanisław
Stankowski Wojciech T. J.
Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
Geologos
iron meteorite
terrestrial age
dosimetry
poland
author_facet Fedorowicz Stanisław
Stankowski Wojciech T. J.
author_sort Fedorowicz Stanisław
title Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
title_short Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
title_full Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
title_fullStr Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
title_full_unstemmed Dating the Morasko meteorite fall by natural thermoluminescence of the fusion crust
title_sort dating the morasko meteorite fall by natural thermoluminescence of the fusion crust
publisher Sciendo
series Geologos
issn 2080-6574
publishDate 2016-09-01
description The 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.
topic iron meteorite
terrestrial age
dosimetry
poland
url https://doi.org/10.1515/logos-2016-0024
work_keys_str_mv AT fedorowiczstanisław datingthemoraskometeoritefallbynaturalthermoluminescenceofthefusioncrust
AT stankowskiwojciechtj datingthemoraskometeoritefallbynaturalthermoluminescenceofthefusioncrust
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