Subducted banded iron formations as a source of ultralow-velocity zones at the core–mantle boundary
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Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature03430.pdf
Reference28 articles.
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2. Williams, Q. & Garnero, E. J. Seismic evidence for partial melt at the base of the mantle. Science 273, 1528–1530 (1996)
3. Knittle, E. & Jeanloz, R. Simulating the core-mantle boundary: an experimental study of high-pressure reactions between silicates and liquid iron. Geophys. Res. Lett. 16, 609–612 (1989)
4. Buffett, B. A., Garnero, E. J. & Jeanloz, R. Sediments at the top of Earth's core. Science 290, 1338–1342 (2000)
5. Polat, A., Hofman, A. W. & Rosing, M. T. Boninite-like volcanic rocks in the 3.7–3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth. Chem. Geol. 184, 231–254 (2002)
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