Abstract
We study seismic noise recorded in the northeast of the Netherlands by
beamforming and by using empirical Green’s functions obtained by seismic interferometry.
From beamforming we found differences in noise directions in different frequency
bands. The main source region for primary microseisms (0.05–0.08 Hz) is in
the west-northwest direction, while the secondary microseisms (0.1–0.14
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