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In the vicinity of the archeological sites, Nakajima et al. (1974) conducted a reconstruction experiment: they reconstructed a kiln which was carefully imitating an excavated kiln of the seventh century and measured paleomagnetic directions from baked clay samples taken from the kiln.
A sample trihedron with checker-box pattern for the 3D reconstruction experiment.
The reconstruction experiment was conducted in Sakai city, Osaka, Japan, on January 1972 (Nakajima et al. 1974).
For the 3D reconstruction experiment, the average RMSE was 14.54 mm while the average reprojection error was 0.22 pixel.
In 1972, a reconstruction experiment of a kiln had been done to reproduce an excavated kiln of the seventh century in Japan.
Because the reconstruction experiment was done after the measurement of the in situ geomagnetic field, we can compare the in situ filed with archeointensity results obtained by the Tsunakawa-Shaw method.
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A minimum size of 50 and 80 kbp for SFs was used in two independent reconstruction experiments.
Our reconstruction experiments demonstrate the effectiveness of our algorithm and design.
The statistical properties depend in particular also on the presence of time reversal invariance in the system, which can be verified independently by time reversal reconstruction experiments.
Meanwhile, practical image reconstruction experiments are also carried out to verify the effectiveness of the simulation results and the optimization criteria.
More details shown in Supplementary Note 1. Reference-assisted chromosome assembly42 reconstruction of predicted chromosome fragments (PCFs) of the BMR genome was performed using a threshold of 50 and 80 kbp to include syntenic fragments (SFs) in two independent reconstruction experiments, respectively (Supplementary Note 2 and Supplementary Table 7).
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