The cross-correlation functions measured at the CaMI Field Research Station

Here are the daily cross-correlation functions calculated from continuous three‐component seismic data recorded using three dense surface arrays of 10 Hz geophones located within a 900×900 m2 area from May to June 2019. To compute day-long stacked noise correlation functions, we adopt a preprocessing workflow similar to the method described by Bensen et al., (2007) and Lin et al., (2013).