A micrometeorite record in Ordovician Durness Group limestones, Isle of Skye

John Parnell, Natalie Salter, Peter West

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Abstract


Samples of mid-Ordovician Durness Group limestone from Skye yield micrometeorites in the magnetic fraction after dissolution in acid. The micrometeorites are concentrated in the upper part of the sequence, in the Arenig Balnakeil and Croisaphuill formations. This finding is consistent with their stratigraphic distribution determined previously in the Durness district. A single sample of contemporaneous limestones from the Highland Border Fault Zone also yielded a micrometeorite. These observations suggest an elevated flux of meteoritic matter, shortly before the greatest concentration of meteorites in the geological record in the mid-Ordovician of Sweden.
Original languageEnglish
Pages (from-to)81-87
Number of pages7
JournalEarth and Environmental Science Transactions of the Royal Society of Edinburgh
Volume106
Issue number2
Early online date27 Apr 2016
DOIs
Publication statusPublished - Jun 2016

Keywords

  • Arenig
  • cosmic spherule
  • meteorite
  • meteoritic flux
  • Scotland

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