Stagnation of subducting slabs in the transition zone due to slow diffusion in majoritic garnet
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo1772.pdf
Reference29 articles.
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2. Fukao, Y., Obayashi, M. & Nakakuki, T. Stagnant slab: A review. Annu. Rev. Earth Planet. Sci. 37, 19–46 (2009).
3. Tetzlaff, M. & Schmeling, H. The influence of olivine metastability on deep subduction of oceanic lithosphere. Phys. Earth. Planet. Inter. 120, 29–38 (2000).
4. Bass, J. D. & Parise, J. B. Deep earth and recent developments in mineral physics. Elements 4, 157–165 (2008).
5. Frost, D. J. The upper mantle and transition zone. Elements 4, 171–176 (2008).
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