A symmetric variational autoencoder separates coherent crustal signal from per-earthquake noise in receiver functions, producing cleaner virtual receiver functions than standard averaging.
Moho depth variation in southern california from teleseismic receiver functions
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Enhanced receiver function imaging of crustal structures using symmetric autoencoders
A symmetric variational autoencoder separates coherent crustal signal from per-earthquake noise in receiver functions, producing cleaner virtual receiver functions than standard averaging.