Structure of the Upper Mantle Under the EPR from Waveform Inversion of Regional Events

Waveform inversions of seismograms recorded at the Mantle Electromagnetic and Tomography (MELT) Experiment ocean bottom seismometer array from regional events with paths following the East Pacific Rise (EPR) require that low shear velocities (

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Bibliographic Details
Published in:Science (American Association for the Advancement of Science) 1998-05, Vol.280 (5367), p.1227-1229
Main Authors: Webb, Spahr C., Forsyth, Donald W.
Format: Article
Language:English
Subjects:
Anisotropy
Conceptual Tempo
Crystalline rocks
Earth
Earth sciences
Earth, ocean, space
Exact sciences and technology
Faults (Geology)
Geology
Igneous and metamorphic rocks petrology, volcanic processes, magmas
Internal geophysics
Love waves
Mantle
Mantle (Geology)
Marine
Measurement
Modeling
Motion
Ocean floor
Oceans
Phase velocity
Rayleigh waves
S waves
Seismological research
Seismology
Solid-earth geophysics, tectonophysics, gravimetry
The MELT Experiment
Upper mantle
Wave velocity
Waveforms
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Description
Summary:Waveform inversions of seismograms recorded at the Mantle Electromagnetic and Tomography (MELT) Experiment ocean bottom seismometer array from regional events with paths following the East Pacific Rise (EPR) require that low shear velocities (
ISSN:0036-8075
1095-9203
DOI:10.1126/science.280.5367.1227