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Partial melting and the low-velocity zone

Anderson, Don L. and Spetzler, Hartmut (1970) Partial melting and the low-velocity zone. Physics of the Earth and Planetary Interiors, 4 (1). pp. 62-64. ISSN 0031-9201.

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The effect of partial melting on the elastic properties of polycrystalline material is a strong function of the shape of the melt zones. If the lowest melting constituents are concentrated in narrow zones, such as grain boundaries, a small amount of melt, ≈ 1%, can easily explain the upper mantle low-velocity zone, for both shear waves and compressional waves. The Eshelby-Walsh theory for the effective elastic moduli for a material with oblate spheroidal inclusions is used to calculate the compressional and shear velocities in a solid matrix with penny-shaped melt zones as a function of melt concentration and aspect ratio. Previous calculations, based on MacKenzie's (1950) and Sato's (1952) results for spherical inclusions, show a very weak dependence of velocity on melt concentration. The Eshelby-Walsh theory satisfactorily explains the velocities in the two-phase ice-brine system.

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Additional Information:© 1970 North-Holland Publishing Company, Amsterdam. Received 8 May 1970. This research was supported by National Science Foundation Grant GA 12703. We would like to thank J. Walsh for a preprint of his paper.
Funding AgencyGrant Number
NSFGA 12703
Issue or Number:1
Record Number:CaltechAUTHORS:20140430-094250057
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Official Citation:Anderson, D. L., & Spetzler, H. (1970). Partial melting and the low-velocity zone. Physics of the Earth and Planetary Interiors, 4(1), 62-64. doi:
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:45350
Deposited By: Jason Perez
Deposited On:30 Apr 2014 23:23
Last Modified:03 Oct 2019 06:29

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