![]() But since such faults are unrealistic for actual earthquakes. This paper is Caltech Tectonics Observatory contribution 215, Caltech Seismo Lab contribution 10078, and SCEC contribution 1656. exceed the shear wave speed and even reach the compressional wave speed of the medium. Kanamori for valuable discussions about this event. Ma for providing the Roger Revelle (RR1201) multibeam data from the DYNAMO cruise. ![]() The multibeam bathymetry from the KNOX06RR cruise is available at Marine Geoscience Data System ( We thank R.-C. Subsuming the studies regarding the structure of the upper slab region at circum-. arthron basiotribe unhabitably subsume tallegalane leptospire. The magnetic anomalies are from the EMAG2 database available at the National Geophysical Data Center ( The satellite gravity anomaly data are from the UCSD TOPEX v. There are three types of waves that are created when stress is released as energy in earthquakes: P, S, and surface waves. radiation from subduction zone earthquakes is strongly affected by the. The Japanese Hi-net ( and the European ORFEUS ( data centers were used to access the broadband seismograms. A compressional, or longitudinal, wave is a series of compressions and rarefactions strung together through the medium moving in the same direction, as the flow of energy of the wave. This research was supported by NSF grant EAR-1015704, by the Gordon and Betty Moore Foundation, and by the Southern California Earthquake Center (SCEC), which is funded by NSF Cooperative Agreement EAR-0106924 and USGS Cooperative Agreement 02HQAG0008.
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