Table S1. Centroid moment tensor solutions for 186 earthquakes. Table headings are as in previous CMT reports (Ekström et al. 2005). δto, δλo, δφo and δho are differences between respective parameters for CMT solutions and hypocentral locations of either ISC or PDE. For a small number of earthquakes, the event time is that determined in our surface wave analysis, since the NEIC did not detect/locate the event.

Figure S1. Revised CMT solutions on left for earthquakes along Eltanin transform system displayed using lower hemisphere, equal-area projections and those in online GCMT catalogue on right. Moment magnitude shown below each solution; dates in years, month, day, hour and minute at top.

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