Archaeomagnetic knowledge of Neolithic in Bulgaria with emphasis on intensity changes

Table S1. Summarized archaeomagnetic determinations of the studied collections. D – magnetic declination after sun compass correction; I – magnetic declination; Fa – archaeointensity value obtained with the corresponding standard deviation (σ) in a temperature interval T_min – T_max using N_PI points; NRM fraction (f); gap factor (g); quality factor (q); maximum angle of deviation (MAD) are also given. In the sample name, the small letters indicate the specimens used for AI determination whereas each sample direction is calculated as an average of two or three specimen' directions after the corresponding cleaning (thermal or AF). Specimens treated in Rennes laboratory are marked in grey.