The natural thermoluminescence of meteorites. VI - Carbon-14, thermoluminescence and the terrestrial ages of meteorites

Details The natural thermoluminescence of meteorites. VI - Carbon-14, thermoluminescence and the terrestrial ages of meteorites The natural thermoluminescence of meteorites. VI - Carbon-14, thermoluminescence and the terrestrial ages of meteorites

Jun 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993metic..28..196b&link_type=abstract

Meteoritics (ISSN 0026-1114), vol. 28, no. 2, p. 196-203.

Computer Science

15

Meteorites, Radioactive Age Determination, Thermoluminescence, Weathering, Atmospheric Entry, Great Plains Corridor (North America), Meteoritic Composition, Sahara Desert (Africa), Temporal Distribution, Meteorites, Thermoluminescence, Carbon, Isotopes, Carbon 14, Catalog, Age, Terrestrial Age, Comparison, Saharan Meteorites, Decay, Procedure, Mass Specrometry, Ams, Laboratory Studies, Samples, Meteorite, Raggane, Parameters, Roosevelt County, Acfer, Daraj, Hammadah Al Hamra, Ilafegh, Tanezrouft, Weathering

Scientific paper

A relationship is noted between the natural thermoluminescence (TL) levels and the C-14-derived terrestrial ages for meteorite finds from the U.S. Prairie States and Roosevelt County, NM; those in the Sahara are also in accord with calculated TL decay curves, for 'storage' temperatures equal to the approximate average annual temperatures at individual sites. This discussion is limited to the empirical correspondence between the two methodologies, and to theoretical decay curves for a single 'average' ordinary chondrite.

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