Two overlapping oceanic plates are sinking into the mantle underneath central Japan where they dehydrate, releasing water-rich fluids that enhance mantle melting. Geochemical work helps determine the relative contribution of each plate to the overall fluid budget.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Nakamura, H., Iwamori, H. & Kimura, J. I. Nature Geosci. 1, 380–384 (2008).
Anderson, R. N., Delong, S. E. & Schwarz W. M. J. Geol. 86, 731–739 (1978).
Hawkesworth, C. J., Gallagher, K., Hergt, J. M. & McDermott, F. Lithos 33, 169–188 (1994).
Cervantes, P. & Wallace, P. J. Geology 31, 235–238 (2003).
Yogodzinski, G. M. et al. Nature 409, 500–504 (2001).
Alexeiev, D. V., Gaedicke, C., Tsukanov, N. V. & Freitag, R. Int. J. Earth Sci. 95, 977–993 (2006).
Ishikawa, T., Tera, F. & Nakazawa, T. Geochim. Cosmochim. Acta 65, 4523–4537 (2001).
Chan, L. H., Leeman, W. P. & You, C. F. Chem. Geol. 160, 255–280 (1999).
Lander, A. V. & Shapiro, M. N. AGU Monograph Series 172, 57–64 (2008).
Dorendorf, F., Wiechert, U. & Wőrner, G. Earth Planet. Sci. Lett. 175, 69–86 (2000).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Churikova, T. Seeing through tectonic plates. Nature Geosci 1, 350–351 (2008). https://doi.org/10.1038/ngeo215
Issue Date:
DOI: https://doi.org/10.1038/ngeo215