Figure 7
From: Detection of oriented fractal scaling components in anisotropic two-dimensional trajectories
DMA results for oscillating time-series. (a) Sinusoidal wave. (b) Second-order auto-regressive (AR(2)) model. (c) Earthquake ground acceleration of the aftershock (Fig. 6). The slopes (\(\approx 1.2\)) in the range smaller than the plateau regime characterise the correlation properties of the noisy fluctuations.
