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Table 1 Selection criteria and threshold values for the three determination classes (A, B, and C) for Thellier–Coe experiments

From: A multimethod paleointensity approach applied to the historical Xitle lava flows (Central Mexico): towards the accurate paleointensity determination

Class

A

B

C

N

≥ 5

≥ 5

≥ 5

σ/slope

≤ 0.10

≤ 0.15

≤ 0.15

f

≥ 0.5

≥ 0.3

≥ 0.3

q

≥ 3

≥ 2

≥ 2

MAD-anc

≤ 5

≤ 10

≤ 10

α

≤ 15

≤ 15

≤ 15

δ(CK)

≤ 5

≤ 9

≤ 15

δ(pal)

≤ 5

≤ 10

≤ 15

δ(TR)

≤ 5

≤ 7

≤ 7

δ(t*)

≤ 3

≤ 30

≤ 30

  1. N, number of points in the Arai plot used for the linear best-fit; σ/slope, the ratio of the standard error of the slope of the selected segment in the Arai plot to the absolute value of the slope; f, NRM fraction used for the best-fit calculation; q, quality factor (Coe et al. 1978); MAD-anc, anchored maximum angular deviation; α, the angular difference between the anchored and non-anchored best-fit; δ(CK), relative check error; δ(pal), cumulative check error (Leonhardt et al. 2004); δ(TR), relative intensity difference in pTRM tail check; δ(t*): the normalized tail of pTRM (Leonhardt et al. 2004)