Correlation of seismic records detects coherently propagating waves from diverse origins, such as the continuous noise field and localised microseisms, the coda of large earthquakes, or repetitive anthropogenic activities (like mining or freight train operation). Although seismic interferometry is frequently approached in terms of Green’s function retrieval, correlation seismology adds a broader perspective by treating interferometric functions (including auto-/cross-correlation and deconvolution) as self-contained observations.

Contributions may include theoretical and numerical developments and applications in correlation seismology, regardless of data type, and covering all scales from superficial structures like sedimentary basins and the cryosphere, to crustal scales and deep structures such as the mantle and the core of the Earth and other seismically monitored planets. We invite abstracts addressing new approaches for correlation-based imaging and monitoring, novel processing strategies, source-structure trade-off and accounting for heterogeneous source distributions.