A role for subducted super-hydrated kaolinite in Earth’s deep water cycle-Reference-Cited by-同舟云学术

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A role for subducted super-hydrated kaolinite in Earth’s deep water cycle

Published:2017-11-20 Issue:12 Volume:10 Page:947-953
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Hwang Huijeong,Seoung Donghoon,Lee Yongjae,Liu Zhenxian,Liermann Hanns-Peter,Cynn Hyunchae,Vogt Thomas,Kao Chi-Chang,Mao Ho-Kwang

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/s41561-017-0008-1.pdf

Reference64 articles.

1. van Keken, P. E., Hacker, B. R., Syracuse, E. M. & Abers, G. A. Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide. J. Geophys. Res. 116, B10401 (2011)

2. Wallace, P. J. Volatiles in subduction zone magmas: concentrations and fluxes based on melt inclusion and volcanic gas data. J. Volcanol. Geoth. Res. 140, 217–240 (2005).

3. Tatsumi, Y. & Eggins, S. Subduction Zone Magmatism (Blackwell Scientific, Oxford, 1995).

4. Mibe, K., Fujii, T. & Yasuda, A. Control of the location of the volcanic front in island arcs by aqueous fluid connectivity in the mantle wedge. Nature 401, 259–262 (1999).

5. Hattori, K. H. & Guillot, S. Volcanic fronts form as a consequence of serpentinite dehydration in the forearc mantle wedge. Geology 31, 525–528 (2003).

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