The cold and relatively dry nature of mantle forearcs in subduction zones
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo2922.pdf
Reference38 articles.
1. Grove, T. L., Till, C. B. & Krawczynski, M. J. The role of H2O in subduction zone magmatism. Annu. Rev. Earth Planet. Sci. 40, 413–439 (2012).
2. Abers, G. A., van Keken, P. E., Kneller, E. A., Ferris, A. & Stachnik, J. C. The thermal structure of subduction zones constrained by seismic imaging: implications for slab dehydration and wedge flow. Earth Planet. Sci. Lett. 241, 387–397 (2006).
3. Wada, I. & Wang, K. Common depth of slab-mantle decoupling: reconciling diversity and uniformity of subduction zones. Geochem. Geophys. Geosyst. 10, Q10009 (2009).
4. Syracuse, E. M., van Keken, P. E. & Abers, G. A. The global range of subduction zone thermal models. Phys. Earth Planet. Int. 183, 73–90 (2010).
5. Reynard, B. Serpentine in active subduction zones. Lithos 178, 171–185 (2013).
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