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Crustal Thickness on the Mid-Atlantic Ridge: Bull's-Eye Gravity Anomalies and Focused Accretion

Tolstoy, Maya, Harding, Alistair J., Orcutt, John A.·1993·Science

Abstract

Spreading segments of the Mid-Atlantic Ridge show negative bull's-eye anomalies in the mantle Bouguer gravity field. Seismic refraction results from 33°S indicate that these anomalies can be accounted for by variations in crustal thickness along a segment. The crust is thicker in the center and thinner at the end of the spreading segment, and these changes are attributable to variations in the thickness of layer 3. The results show that accretion is focused at a slow-spreading ridge, that axial valley depth reflects the thickness of the underlying crust, and that along-axis density variations should be considered in the interpretation of gravity data.

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Metadata

Authors
Tolstoy, M., Harding, A. J., & Orcutt, J. A.
Venue
Science
Published
1993-10-29
Volume
262
Issue
5134
Pages
726-729
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2068473785
Cited by
270
References
0
FWCI
25.94
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Crustal Thickness on the Mid-Atlantic Ridge: Bull's-Eye Gravity Anomalies and Focused Accretion. https://app.cochat.ai/papers/10.1126/science.262.5134.726
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Tolstoy, M., Harding, A. J., & Orcutt, J. A. (1993). Crustal Thickness on the Mid-Atlantic Ridge: Bull's-Eye Gravity Anomalies and Focused Accretion. Science. https://doi.org/10.1126/science.262.5134.726

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.