Figure 2
From: Imaging and seismic modelling inside volcanoes using machine learning
40 synthetic seismic sensors are distributed across the surface of all models. The seismogram amplitudes are normalised. This example shows synthetic vertical seismic traces for the sample from population L in panel (A) and population T in panel (B). See also Fig. 1. A random selection of 10 sensors is used in FNO training.
