The behavior of Li and B isotopes in high-T and low-T eclogites enclosed by phengite schists
Author:
Funder
National Natural Science Foundation of China
Basic Research Foundation of the CAGS
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00410-024-02124-1.pdf
Reference113 articles.
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3. Andrews E, Pogge von Strandmann PAE, Fantle MS (2020) Exploring the importance of authigenic clay formation in the global Li cycle. Geochim Cosmochim Acta 289:47–68. https://doi.org/10.1016/j.gca.2020.08.018
4. Barnes JD, Cullen J, Barker S, Agostini S, Penniston-Dorland S, Lassiter JC, Klügel A, Wallace L (2019) The role of the upper plate in controlling fluid-mobile element (Cl, Li, B) cycling through subduction zones: Hikurangi forearc, New Zealand. Geosphere 15:642–658. https://doi.org/10.1130/GES02057.1
5. Bebout GE, Barton MD (1989) Fluid flow and metasomatism in a subduction zone hydrothermal system: catalina Schist terrane, California. Geology 17:976–980. https://doi.org/10.1130/0091-7613(1989)017/3C0976:FFAMIA/3E2.3.CO;2
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