Computes the geometric mean composition of a set of fission track or U-Th-He data and returns the corresponding age and fitting parameters.
central(x, ...)# S3 method for default
central(x, ...)
# S3 method for UThHe
central(x, ...)
# S3 method for fissiontracks
central(x, mineral = NA, ...)
an object of class UThHe
or fissiontracks
,
OR a 2-column matrix with (strictly positive) values and
uncertainties
optional arguments
setting this parameter to either apatite
or
zircon
changes the default efficiency factor, initial
fission track length and density to preset values (only affects
results if x$format=2
.)
a list containing the following items:
the reduced Chi-square statistic of data concordance,
i.e. \(mswd=SS/(2n-2)\), where \(SS\) is the sum of squares
of the log[U/He]-log[Th/He] compositions and \(n\) is the number
of samples. If x
has class fissiontracks
, then
\(mswd=X^2/(n-1)\), where \(X^2\) is a Chi-square statistic of
the EDM data or ICP ages.
the p-value of a Chi-square test with \(n-2\) degrees of freedom
a two-column vector with the central age and its standard error.
Additionally, if x
has class UThHe
:
(if the input data table contains Sm) or uv (if it doesn't): the geometric mean log[U/He], log[Th/He] (, log[Sm/He]) and log[Sm/He] composition
the covariance matrix of uvw
or uv
OR, if x
has class fissiontracks
:
the (over)dispersion of the ages (value between 0 and 1)
Galbraith, R.F. and Laslett, G.M., 1993. Statistical models for mixed fission track ages. Nuclear tracks and radiation measurements, 21(4), pp.459-470.
Vermeesch, P., 2008. Three new ways to calculate average (U-Th)/He ages. Chemical Geology, 249(3), pp.339-347.
# NOT RUN {
data(examples)
print(central(examples$UThHe)$age)
# }
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