Model-Based Identification of the Base of the Gas Hydrate Stability Zone in Multichannel Reflection Seismic Data, Offshore Costa Rica
The magnitudes of the reflection coefficients for the seafloor reflection and the BSR are calculated for a model with 3% free gas below the gas hydrate stability zone . Density and seismic velocities are taken from the full-waveform inversion of Pecher et al. . The black boxes mark the incident angle ranges which are shown in Figure 6.
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