S-to-P Conversions from Mid-mantle Slow Scatterers in Slab Regions: Observations of Deep/Stagnated Oceanic Crust?
Author:
Funder
NSFC
State Key Laboratory of Marine Geology, Tongji University
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00024-017-1763-z/fulltext.html
Reference56 articles.
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2. Ballmer, M. D., Houser, C., Hernlund, J. W., Wentzcovitch, R. M., & Hirose, K. (2017). Persistence of strong silica-enriched domains in the Earth’s lower mantle. Nature Geoscience, 10(3), 236–240. https://doi.org/10.1038/NGEO2898 .
3. Bentham, H., & Rost, S. (2014). Scattering beneath western Pacific subduction zones: evidence for oceanic crust in the mid-mantle. Geophysical Journal International, 197, 1627–1641.
4. Bentham, H. L. M., Rost, S., & Thorne, M. S. (2017). Fine-scale structure of the mid-mantle characterised by global stacks of PP precursors. Earth and Planetary Science Letters, 472, 164–173.
5. Castle, J. C., & Creager, K. C. (1999). A steeply dipping discontinuity in the lower mantle beneath Izu-Bonin. Journal of Geophysical Research: Solid Earth, 104(B4), 7279–7292.
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