Fig. 7: Marginal probability density distributions resulting from the inversion of balloon data.
From: Balloon seismology enables subsurface inversion without ground stations
Distributions of a origin time and latitude, b origin time and longitude, c first layer thickness and shear wave velocity, d third layer thickness and shear wave velocity, e Poisson’s ratio and shear wave velocity in the fifth layer, and f shear wave velocities in the first and second layer. A darker hue represents a higher density of models.
