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A Parallel Evolution Strategy for an Earth Imaging Problem in Geophysics

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Academic year: 2021

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Figure 1: Acoustic waves propagated by a source are reflected by a reflective layer (in white) and are detected by the geophones
Figure 2 depicts a graphical representation of the SEG 1 /EAGE 2 salt dome velocity model (described later in Section 2.3) and the real part of the wavefield at frequency 12 Hz obtained after solving the Helmholtz equation in the case of a single source
Figure 3: Visualization of the 3D SEG/EAGE salt dome velocity model using ParaView [24]
Figure 4: Illustration using 1D SEG/EAGE salt dome velocity profiles.
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