The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Water-Induced Fabric Transitions in Olivine
Abstract
The interpretation of seismic anisotropy in Earth's upper mantle has traditionally been based on the fabrics (lattice-preferred orientation) of relatively water-poor olivine. Here we show that when a large amount of water is added to olivine, the relation between flow geometry and seismic anisotropy undergoes marked changes. Some of the puzzling observations of seismic anisotropy in the upper mantle, including the anomalous anisotropy in the central Pacific and the complicated anisotropy in subduction zones, can be attributed to the enrichment of water in these regions.
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Hirth, G., & Kohlstedt, D. L. (1996) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(96)00154-9 · Cited by 1,599
Cited by
Subduction factory: 4. Depth-dependent flux of H 2 O from subducting slabs worldwide
van Keken, P. E., Hacker, B. R., Syracuse, E. M., & Abers, G. A. (2011) · Journal of Geophysical Research · doi:10.1029/2010jb007922 · Cited by 949
Effects of pressure on high-temperature dislocation creep in olivine
Karato, S.-I., & Jung, H. (2003) · Philosophical Magazine · doi:10.1080/0141861021000025829 · Cited by 420
Self-citation
Metadata
- Authors
- Jung, H., & Karato, S.-I.
- Venue
- Science
- Published
- 2001-08-24
- Volume
- 293
- Issue
- 5534
- Pages
- 1460-1463
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2062018184
- Cited by
- 852
- References
- 1
- FWCI
- 21.20
- Type
- journal article
- Language
- en
- Open access
- closed
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