Earthquakes along Eltanin transform system, SE Pacific Ocean: fault segments characterized by strong and poor seismic coupling and implications for long-term earthquake prediction
Article first published online: 9 DEC 2011
© 2011 The Authors Geophysical Journal International © 2011 RAS
Geophysical Journal International
Volume 188, Issue 2, pages 421–434, February 2012
How to Cite
Sykes, L. R. and Ekström, G. (2012), Earthquakes along Eltanin transform system, SE Pacific Ocean: fault segments characterized by strong and poor seismic coupling and implications for long-term earthquake prediction. Geophysical Journal International, 188: 421–434. doi: 10.1111/j.1365-246X.2011.05284.x
- Issue published online: 5 JAN 2012
- Article first published online: 9 DEC 2011
- Accepted 2011 October 25. Received 2011 October 20; in original form 2011 August 16
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 www.globalcmt.org/CMTsearch.html on right. Moment magnitude shown below each solution; dates in years, month, day, hour and minute at top.
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