Distribution of rare earth elements and uranium in various components of ordinary chondrites

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Chemical Fractionation, Chondrites, Meteoritic Composition, Neutron Activation Analysis, Rare Earth Elements, Uranium, Calcium Phosphates, Colorimetry, Leaching, Meteorites, Rare Earth Elements, Distribution, Uranium, Composition, Ordinary Chondrites, Kesen, Richardton, Bruderheim, St. Severin, H Chondrites, L Chondrites, Ll Chondrites, Procedure, Phases, Data, Fractionation, Neutron Activation Analysis, Fission Tracks, Origin, Enrichment, Calcium, Phosphate, Minerals, Chemistry, Source, Formation, Metamorp

Scientific paper

Rare earth elements (REE) and uranium were studied for their distributions in various component phases of four ordinary chondrites. Kesen (H4), Richardton (H5), Bruderheim (L6), and Saint Severin (LL6). A selective dissolution method was applied for the phase fractionation. The REE were analysed by neutron activation analysis, and U was determined by neutron-induced fission tracks. The present study revealed that both REE and U are highly enriched in the Ca-phosphate minerals with different enrichment factors, implying chemical fractionation between them. The phosphates seem to be responsible for more than 80 percent of the light REE in all chondrites. On the other hand, only 20-40 percent of the total U resides in the Ca-phosphates. This difference in enrichments might have been caused through the levels of metamorphic activity on the meteoritic parent bodies.

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