massfractionation

Applies the fractionation obtained from air shot data by
<code>fractionation</code> to the denominator detector in order to
correct it for the mass difference between the numerator and
denominator isotopes.

Processes noble gas mass spectrometer data to determine the isotopic composition of argon (comprised of Ar36, Ar37, Ar38, Ar39 and Ar40) released from neutron-irradiated potassium-bearing minerals. Then uses these compositions to calculate precise and accurate geochronological ages for multiple samples as well as the covariances between them. Error propagation is done in matrix form, which jointly treats all samples and all isotopes simultaneously at every step of the data reduction process. Includes methods for regression of the time-resolved mass spectrometer signals to t=0 ('time zero') for both single- and multi-collector instruments, blank correction, mass fractionation correction, detector intercalibration, decay corrections, interference corrections, interpolation of the irradiation parameter between neutron fluence monitors, and (weighted mean) age calculation. All operations are performed on the logs of the ratios between the different argon isotopes so as to properly treat them as 'compositional data', sensu Aitchison [1986, The Statistics of Compositional Data, Chapman and Hall].

Pieter Vermeesch

ArArRedux

Rigorous Data Reduction and Error Propagation of Ar40 / Ar39
Data

massfractionation function

<dl><dt>X</dt>
<dd>an object of class <code>redux</code></dd>
<dt>fract</dt>
<dd>a list with fractionation data for Ar37, Ar39 and Ar40</dd></dl>

Arguments

Apply the mass fractionation correction — massfractionation

<dl>

<dt>X</dt>
<dd>an object of class <code>redux</code></dd>


<dt>fract</dt>
<dd>a list with fractionation data for Ar37, Ar39 and Ar40</dd>

</dl>

massfractionation: Apply the mass fractionation correction

Description

Usage

Value

Arguments

Examples