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A pTRM check is a repeat TRM acquisition step to test for changes in a specimen's ability to acquire TRM at blocking temperatures below the temperature of the check. difference between a pTRM check and the original TRM is calculated as the scalar intensity difference. That is, δpTRMi,j=pTRM_checki,j−TRMi=pTRM_checki,j−xi, where pTRM_checki,j is the pTRM check to the ith temperature step after heating to the jth temperature step. The order of the difference is such that pTRM checks smaller than the original TRM yield negative δpTRMi,j and pTRM checks larger than the original TRM give positive δpTRMi,j. For a pTRM check to be included in the analysis, both Ti and Tj must be less than or equal to Tmax.
Statistic: npTRM
The number of pTRM checks used to analyze the best-fit segment on the Arai plot (i.e., the number of pTRMi,j with Ti≤Tmax and Tj≤Tmax).
Statistic: check(%)
Report to 1 d.p.
Maximum absolute difference produced by a pTRM check, normalized by the TRM acquired at that heating step. check(%)=max{|δpTRMi,j|xi×100}i≤end and j≤end
Statistic: δCK
Report to 1 d.p.
Maximum absolute difference produced by a pTRM check, normalized by the total TRM (obtained from the intersection of the best-fit line and the x-axis on an Arai plot; Leonhardt et al., 2004a). δCK=max{|δpTRMi,j|}i≤end and j≤end|XInt.|×100
Statistic: DRAT
Report to 1 d.p.
Maximum absolute difference produced by a pTRM check, normalized by the length of the best-fit line (Selkin and Tauxe, 2000). DRAT=max{|δpTRMi,j|}i≤end and j≤endL×100, where L is the length of the best-fit line on the Arai plot. L is given by: L=√(Δx′)2+(Δy′)2, where Δx′ and Δy′ are TRM and NRM lengths of the best-fit line on the Arai plot, respectively (Section 3).
Statistic: maxDEV
Report to 1 d.p.
Maximum absolute difference produced by a pTRM check, normalized by the length of the TRM segment of the best-fit line on the Arai plot (Blanco et al., 2012). maxDEV=max{|δpTRMi,j|}i≤end and j≤endΔx′×100
Most cumulative pTRM checks can be calculated in two fashions. The first method, is the summation of the signed pTRM differences (i.e., ±δpTRM), the second is to calculate the sum of the absolute pTRM difference (i.e., |δpTRM|). The convention of the Standard Paleointensity Definition is to denote the second approach with a prime (′). For example, CDRAT is calculated by the first method and CDRAT′ by the second.
Statistic: CDRAT
Report to 1 d.p.
Cumulative DRAT (Kissel and Laj, 2004). CDRAT=|end∑i=1δpTRMi,j|L×100 CDRAT′=end∑i=1|δpTRMi,j|L×100
Statistic: DRATS
Report to 1 d.p.
Cumulative pTRM check difference normalized by the pTRM gained at the maximum temperature used for the best-fit on the Arai diagram (Tauxe and Staudigel, 2004). DRATS=|end∑i=1δpTRMi,j|xend×100 DRATS′=end∑i=1|δpTRMi,j|xend×100
Statistic: Mean DRAT
Report to 1 d.p.
The average difference produced by a pTRM check, normalized by the length of the best-fit line. Mean DRAT=1npTRM|end∑i=1δpTRMi,j|L×100 Mean DRAT′=1npTRMend∑i=1|δpTRMi,j|L×100
Statistic: Mean DEV
Report to 1 d.p.
Mean deviation of a pTRM check (Blanco et al., 2012). Mean DEV=1npTRM|end∑i=1δpTRMi,j|Δx′×100 Mean DEV′=1npTRMend∑i=1|δpTRMi,j|Δx′×100.
Statistic: δpal
Report to 1 d.p.
A measure of cumulative alteration determined by the difference of the alteration corrected intensity estimate (Valet et al., 1996) and the uncorrected estimate, normalized by the uncorrected estimate (Leonhardt et al., 2004a).
We first calculate the cumulative sum of the pTRM checks up to the ith step of the experiment:
Ci=l=i∑l=1δpTRMl,j, for i=1,…,nmax,
where δpTRMl,j is the vector difference between TRMl and pTRM_checkl,j, i.e.,
δpTRMl,j=TRMl−pTRM_checkl,j.
When no pTRM check is performed δpTRMl=[0,0,0].
The TRMi vector is then corrected by adding the cumulative effect of the alteration, Ci:
TRM∗i=TRMi+Ci, for i=1,…,nmax.
Since no pTRM check is performed at the first step:
TRM∗1=TRM1.
The corrected TRM values on the Arai plot (x∗i) can be calculated by determining the vector lengths of TRM∗i. The corrected slope on the Arai plot (b∗) can be calculated using the selected points and the standard approach outlined in Section 3. δpal is then given by: δpal=|b−b∗b|×100.
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