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Imaging the Deep Seismic Structure Beneath a Mid-Ocean Ridge: The MELT Experiment

Team, The MELT Seismic·1998·Science

Abstract

The Mantle Electromagnetic and Tomography (MELT) Experiment was designed to distinguish between competing models of magma generation beneath mid-ocean ridges. Seismological observations demonstrate that basaltic melt is present beneath the East Pacific Rise spreading center in a broad region several hundred kilometers across and extending to depths greater than 100 kilometers, not just in a narrow region of high melt concentration beneath the spreading center, as predicted by some models. The structure of the ridge system is strongly asymmetric: mantle densities and seismic velocities are lower and seismic anisotropy is stronger to the west of the rise axis.

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Metadata

Authors
Team, T. M. S.
Venue
Science
Published
1998-05-22
Volume
280
Issue
5367
Pages
1215-1218
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W4366065132
Cited by
332
References
0
FWCI
16.32
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Imaging the Deep Seismic Structure Beneath a Mid-Ocean Ridge: The MELT Experiment. https://app.cochat.ai/papers/10.1126/science.280.5367.1215
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Team, T. M. S. (1998). Imaging the Deep Seismic Structure Beneath a Mid-Ocean Ridge: The MELT Experiment. Science. https://doi.org/10.1126/science.280.5367.1215

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