Upper-mantle seismic discontinuities and the thermal structure of subduction zones
The precise depths at which seismic velocities change abruptly in the upper mantle are revealed by the analysis of data from hundreds of seismometers across the western United States. The boundary near 410 km depth is locally elevated, that near 660 km depressed. The depths of these boundaries, which mark phase transitions, provide an in situ thermometer in subduction zones: the observed temperature contrasts require at least moderate thickening of the subducting slab near 660 km depth. In addition, a reflector near 210 km depth may mark the bottom of the aesthenosphere.
Citation Information
Publication Year | 1992 |
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Title | Upper-mantle seismic discontinuities and the thermal structure of subduction zones |
Authors | J.E. Vidale, H. M. Benz |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Nature |
Index ID | 70017163 |
Record Source | USGS Publications Warehouse |