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CONTRIBUTION TO THE DATING OF IRON METEORITES BY THE RHENIUM-OSMIUM METHOD (in German)

Journal Article · · Z. Naturforsch
OSTI ID:4809618
The rhenium and osmium contents and the isotopic compositions of osmium in a number of meteorites were measured. Os./Re ratios and Os/sup 187/Os/sup 186/ ratios vary sufficiently to make the Re/sup 187/Os/sup 187/ dating-method appllcable to meteorites. Also, the isotopic compositions of several samples of common terrestrial osmium were determined, giving variations in the Os/sup187/Os/ sup 186/ ratio which are larger than the common terrestrial strontium variations. The half life of Re/sup 187/ still is only tentatively known. Taking the latest value (4.3 x 10/sup 10/ years), it is shown that the results are in agreement with the assumption that stone meteorites, iron meteorites, and the crust of the earth were formed about 4 to 5 AE ago. (auth)
Research Organization:
Universitat, Cologne; and Max-Planck-Institut fur Chemie, Mainz
NSA Number:
NSA-16-010751
OSTI ID:
4809618
Journal Information:
Z. Naturforsch, Journal Name: Z. Naturforsch Vol. Vol: 16a
Country of Publication:
Country unknown/Code not available
Language:
German

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