The use of waveform cross correlation to recover the aftershock sequence of the August 14, 2016 earthquake within Sakhalin Island
The method of waveforms cross correlation (WCC) is used to detect signals from aftershocks of the August 14, 2016 earthquake within Sakhalin Island, which had local magnitude ML = 6.1. Arrivals of regular P- and S-waves detected by the WCC method with various master events at 6 regional stations are associated into a set of seismic events called the cross correlation standard event list (XSEL). We compare the XSEL with the bulletin for the same aftershock sequence compiled in routine seismological processing. The principal advantage of the XSEL is expressed in the increasing number of found seismic events with three or more associated stations, a slight decrease in the magnitude threshold of catalogue completeness, and more accurate location of the epicentres for even the smallest aftershocks. The improved aftershock locations tend to cluster in a narrow zone corresponding to the western board of the Central Sakhalin fault, which defines the boundary between the Okhotsk and the Eurasian (Amur) slabs.