Joint ambient noise autocorrelation and receiver function analysis of the Moho

In the field of seismic interferometry, cross-correlations are used to extract Green's function from ambient noise data. By applying a single station variation of the method, using autocorrelations, we are in principle able to retrieve zero-offset reflections in a stratified Earth. These reflections are valuable as they do not require an active seismic source and, being zero-offset, are better con...