Metasomatism at a metapelite–ultramafic rock contact at the subduction interface: Insights into mass transfer and fluid flow at the mantle wedge corner
Author:
Funder
Japan Society for the Promotion of Science
the University of Tokyo
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-023-02011-1.pdf
Reference111 articles.
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2. Ague JJ (2014) Fluid flow in the deep crust. Treatise on geochemistry, 2nd edn. Elsevier, Amsterdam, pp 203–247
3. Aoya M, Endo S, Mizukami T, Wallis SR (2013) Paleo-mantle wedge preserved in the Sambagawa high-pressure: metamorphic belt and the thickness of forearc continental crust. Geology 41:451–454. https://doi.org/10.1130/G33834.1
4. Banno S (2004) Ultramafic rocks and associated eclogites of the Sanbagawa Schists, Japan: a review. Int Geol Rev 46:693–704. https://doi.org/10.2747/0020-6814.46.8.693
5. Banno S, Sakai C, Higashino T (1986) Pressure-temperature trajectory of the Sanbagawa metamorphism deduced from garnet zoning. Lithos 19:51–63. https://doi.org/10.1016/0024-4937(86)90015-0
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