Refining the high-fidelity archaeointensity curve for Western Europe over the past millennium: Analysis of Tuscan architectural bricks (Italy)
Agnès Genevey
Claudia Principe
Yves Gallet
Giuseppe Clemente
Maxime Le Goff
Alexandre Fournier
Pasquino Pallecchi
10.6084/m9.figshare.10265180.v1
https://geolsoc.figshare.com/articles/journal_contribution/Refining_the_high-fidelity_archaeointensity_curve_for_Western_Europe_over_the_past_millennium_Analysis_of_Tuscan_architectural_bricks_Italy_/10265180
Supplementary table 2: Intensity results obtained at the specimen level and mean values obtained at the fragment level. `Tmin-Tmax': Interval of temperature involved for the intensity computation. `Flab': Intensity of the laboratory field in µT. `NRM T1 (T1')' column: Percentage of magnetisation fraction with unblocking temperatures larger than T1 (or T1'). `Slope R': Slope of the straight line computed from the R'(Ti) data between Tmin and Tmax. `F Triaxe': Intensity values obtained at the specimen level in µT. `F Triaxe mean value per fragment ± σ F': Mean intensity value obtained at the fragment level with its standard error when computed from 2 values or its standard deviation when computed from 3 values. *: (n1/n2/n3) indicates successively the number of fragments collected, the number of fragments whose magnetization was strong enough relative to the Triaxe sensitivity and the number of fragments retained to estimate a mean value at the group level.
2019-11-07 10:40:28
Intensity
fragment level
µ T
specimen level
Triaxe
NRM T 1
high-fidelity archaeointensity curve
Geology