Seismological mapping of fine structure near the base of the Earth's mantle
Nature
By: J.E. Vidale and H. M. Benz
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Abstract
THE Earth's core-mantle boundary (CMB) juxtaposes liquid iron and crystalline silicates, and is a region of large vertical thermal gradients. The D??? region, which extends up to 200-300 km above the CMB, often has elevated shear-wave velocity and suggestions of lateral variations in structure1. Recent improvements in our ability to assemble and analyse records from regional seismic networks have allowed us to examine long profiles of travel times, amplitudes and waveforms from more than a thousand short-period seismometers2. We observe, across Canada and the United States, P waves that have grazed the CMB from the powerful nuclear test in Lop Nor, China, on 21 May 1992. First-arrival travel times and large secondary arrivals are consistent with a 1.5% compressional velocity increase with depth ???130 km above the CMB - about half the thickness of D??? in this locality3. Our observations, together with evidence for the absence of such a thin, fast layer in neighbouring regions, suggest the presence of lateral heterogeneity in composition or phase at the base of the mantle.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Seismological mapping of fine structure near the base of the Earth's mantle |
| Series title | Nature |
| Volume | 361 |
| Issue | 6412 |
| Year Published | 1993 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Nature |
| First page | 529 |
| Last page | 532 |
| Google Analytic Metrics | Metrics page |