Fractionation and dating updating do records

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Uncleaved Welsh mudrocks of the diagenetic zone yield Sm-Nd leachate-residue ages of 453–484 Ma, in agreement with their Llanviian to Caradocian biostratigraphic ages, whereas higher grade rocks of the anchizone and epizone yield Sm-Nd ages as young as 413 Ma.

These ages are transitional between the time of deposition and the time of regional deformation related to the Acadian Orogeny at 390 Ma.

The ratio is measured using an ordinary mass spectrometer.

The isotopic composition of the sample being measured is expressed as delta13C which represents the parts per thousand difference (per mille) between the sample carbon 13 content and the content of the international PDB standard carbonate (Keith et al., 1964; Aitken, 1990).

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