Figure 4 | Scientific Reports

Figure 4

From: Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization

Figure 4

(a) Autocorrelation image from oceanic microseism noise. (b) The separated scattered Scholte waves from autocorrelation profile. (c) Magnitude 3.4 Gilroy earthquake wavefield observed on DAS cable on 11 March 2018. (A) The black dashed lines indicates the observed horizontal discontinuities. The fuchsia dashed lines indicate the apparent velocities of the scattered arrivals.

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