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Earth, Planets and Space

Table 7 Acceptable results of the IZZI-Thellier experiment

From: Archeointensity estimates of a tenth-century kiln: first application of the Tsunakawa–Shaw paleointensity method to archeological relics

Specimen

NRM0 (A/m)

T1 − T2 (°C)

FRAC

SCAT

GAP-MAX

β

MAD (°)

DANG (°)

Hpast (μT)

BH5G

0.968

200–565

0.98

Pass

0.18

0.039

2.9

1.8

43.3

BH5H

0.597

200–600

0.99

Pass

0.22

0.020

3.2

1.7

50.3

BH7L

1.49

200–600

0.99

Pass

0.23

0.022

2.5

1.6

42.3

Average (Hpast) = 45.3 ± 4.4

  1. T1 − T2, the selected temperature range; H past , the estimated paleointensity
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