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(1997) Discussion on Sm–Nd isotopic age of Precambrian–Cambrian boundary in China. Geological Magazine, 134 (4) 571-574 doi:10.1017/s0016756897007474

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Reference TypeJournal (article/letter/editorial)
TitleDiscussion on Sm–Nd isotopic age of Precambrian–Cambrian boundary in China
JournalGeological Magazine
Year1997 (July)Volume134
Issue4
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756897007474Search in ResearchGate
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Mindat Ref. ID257438Long-form Identifiermindat:1:5:257438:1
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Full Reference(1997) Discussion on Sm–Nd isotopic age of Precambrian–Cambrian boundary in China. Geological Magazine, 134 (4) 571-574 doi:10.1017/s0016756897007474
Plain Text(1997) Discussion on Sm–Nd isotopic age of Precambrian–Cambrian boundary in China. Geological Magazine, 134 (4) 571-574 doi:10.1017/s0016756897007474
In(1997, July) Geological Magazine Vol. 134 (4) Cambridge University Press (CUP)
Abstract/NotesM. J. M. Turnbull & S. Moorbath comment: The paper
of Yang

et al. (1996) describes a novel dating approach, using the Sm–Nd


method on phosphatic material, to determine the age of the

Precambrian–Cambrian boundary. The dates reported are of a precision


which, in light of the relatively small range of

147Sm/144 Nd ratios (0.09–0.17), is

surprising. We have recalculated the published data using the ISOPLOT

program of Ludwig (1991) and this is shown

below in Table 1. These results cast considerable doubt on the

statistical analysis of Yang et al. (1996). While this technique


may have utility with Precambrian successions it would appear

to be of limited use for the high precision dating required for

Phanerozoic stratigraphic correlation.


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