Description Usage Arguments Details Value Author(s) See Also Examples

Returns the predicted *{}^{206}*Pb/*{}^{238}*U and
*{}^{207}*Pb/*{}^{235}*U ratios for any given time with or
without initial U-series disequilibrium.

1 |

`tt` |
the age of the sample |

`d` |
an object of class diseq |

`exterr` |
propagate the uncertainties associated with decay
constants and the |

U decays to Pb in 14 (for *{}^{238}*U) or 11/12 (for
*{}^{235}*U) steps. Conventional U-Pb geochronology assumes
that secular equilibrium between all the short lived intermediate
daughters was established at the time of isotopic closure. Under
this assumption, the relative abundances of those intermediate
daughters can be neglected and the age equation reduces to a simple
function of the measured Pb/U ratios. In reality, however, the
assumption of initial secular equilibrium is rarely met. Accounting
for disequilibrium requires a more complex set of age equations,
which are based on a coupled system of differetial equations. The
solution to this system of equations is given by a matrix
exponential. `IsoplotR`

solves this matrix exponential for any
given time, using either the assumed initial activity ratios, or
(for young samples) the measured activity ratios of the longest
lived intermediate daughters. Based on a `Matlab`

script by
Noah McLean.

a list containing the predicted *{}^{206}*Pb/*{}^{238}*U,
*{}^{207}*Pb/*{}^{235}*U and
*{}^{207}*Pb/*{}^{206}*Pb ratios at time `tt`

; the
derivatives of the *{}^{206}*Pb/*{}^{238}*U,
*{}^{207}*Pb/*{}^{235}*U and
*{}^{207}*Pb/*{}^{206}*Pb ratios with respect to time; and
the derivatives of the *{}^{206}*Pb/*{}^{238}*U,
*{}^{207}*Pb/*{}^{235}*U and
*{}^{207}*Pb/*{}^{206}*Pb ratios with respect to the
intermediate decay constants and
*{}^{238}*U/*{}^{235}*U-ratio.

Noah McLean (algorithm) and Pieter Vermeesch (code)

1 2 3 |

Embedding an R snippet on your website

Add the following code to your website.

For more information on customizing the embed code, read Embedding Snippets.