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Mantle flow at a slab edge: Seismic anisotropy in the Kamchatka Region
Open accessAbstract
The junction of the Aleutian Island and the Kamchatka peninsula defines a sharp turn in the boundary of the Pacific and North American plates, terminating the subduction zones of the northwest Pacific. The regional pattern of shear‐wave birefringence near the junction indicates that trench‐parallel strain follows the seismogenic Benioff zone, but rotates to trench‐normal beyond the slab edge. Asthenospheric mantle is inferred to flow around and beneath the disrupted slab edge, and may influence the shallowing dip of the Benioff zone at the Aleutian junction.
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Citations
Cited by
A Complex Pattern of Mantle Flow in the Lau Backarc
Smith, G. P., Wiens, D. A., Fischer, K. M., Dorman, L. M., Webb, S. C., & Hildebrand, J. A. (2001) · Science · doi:10.1126/science.1058763 · Cited by 274
Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edge
Jadamec, M. A., & Billen, M. I. (2010) · Nature · doi:10.1038/nature09053 · Cited by 254
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy
Ben‐Mansour, W., Wiens, D. A., Mark, H. F., Russo, R. M., Richter, A., Marderwald, E., & Barrientos, S. (2022) · Geophysical Research Letters · doi:10.1029/2022gl099871 · Cited by 20
Metadata
- Authors
- Peyton, V., Levin, V., Park, J., Brandon, M., Lees, J., Gordeev, E., & Ozerov, A.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2001-01-15
- Volume
- 28
- Issue
- 2
- Pages
- 379-382
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2106812239
- Cited by
- 168
- References
- 0
- FWCI
- 6.20
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Peyton, V., Levin, V., Park, J., Brandon, M., Lees, J., Gordeev, E., & Ozerov, A. (2001). Mantle flow at a slab edge: Seismic anisotropy in the Kamchatka Region. Geophysical Research Letters. https://doi.org/10.1029/2000gl012200
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