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Absolute age of formation of chondrites studied by the 87Rb–87Sr method

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Abstract

The 87Rb–87Sr isochrons for H-, E- and LL-, chondrites are undistinguishable from each other. The joint isochron yields an age of 4,498 ± 15 Myr if the rubidium decay constant λ 87Rb = 1.42×10−11 yr−1, and a strontium initial ratio 87Rb/87Sr = 0.69885±0.00010. For the age to agree with U–Th–Pb data, λ 87Rb would have to be changed to 1.402±0.008×10−11 yr−1

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  1. Laboratoire de Géochimie et de Cosmochimie, Département des Sciences de la Terre, Institut de Physique du Globe de Paris, Universités Pierre et Marie Curie et Paris VII, 4, Place Jussieu-75230, Paris, Cedex 05, France

    J-F. Minster, J-L. Birck & C. J. Allègre

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  1. J-F. Minster
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  2. J-L. Birck
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  3. C. J. Allègre
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Minster, JF., Birck, JL. & Allègre, C. Absolute age of formation of chondrites studied by the 87Rb–87Sr method. Nature 300, 414–419 (1982). https://doi.org/10.1038/300414a0

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