Fig. 4From: Exploring planets and asteroids with 6DoF sensors: Utopia and realismActive seismic signals on the moon. Translational acceleration signal recorded after the detonation of 454Â g of explosive in a distance of 1.2Â km from the Apollo17 geophone array (top panel) and the corresponding array-derived rotation rate (bottom panel), bandpass-filtered between 3 and 7Â HzBack to article page