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Elevated flux of cosmic spherules (micrometeorites) in Ordovician rocks of the Durness Group, NW Scotland
Stockholm University, Faculty of Science, Department of Geological Sciences.
2010 (English)In: Scottish Journal of Geology, ISSN 0036-9276, E-ISSN 2041-4951, Vol. 46, 7-16 p.Article in journal (Refereed) Published
Abstract [en]

Limestone samples from the Cambro-Ordovician Durness Group were crushed, acid-digested and searched for evidence of micrometeorites. Eleven melted micrometeorites were extracted from the magnetic fraction of samples from the Balnakeil and Croisaphuill formations near the top of the group. Other formations in the Durness Group did not yield micrometeorites. Only melted spherules with a distinctive dendroidal crystalline structure (I-type cosmic spherules) were accepted as definite micrometeorites. They represent a flux of micrometeorites one to two orders of magnitude greater than at present. The micrometeorite-bearing formations are of Arenig age, coincident with the onset of an enhanced flux of extraterrestrial material identified by the occurrence of fossil meteorites in Sweden.

Place, publisher, year, edition, pages
2010. Vol. 46, 7-16 p.
National Category
Earth and Related Environmental Sciences
Identifiers
URN: urn:nbn:se:su:diva-50657DOI: 10.1144/0036-9276/01-394ISI: 000278428400002OAI: oai:DiVA.org:su-50657DiVA: diva2:383207
Note
authorCount :4Available from: 2011-01-04 Created: 2010-12-30 Last updated: 2017-12-11Bibliographically approved

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