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The behavior of Li and B isotopes in high-T and low-T eclogites enclosed by phengite schists

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Abstract

Subduction zones are critical sites for recycling of Li and B into the mantle. The way of redistribution of Li and B and their isotopes in subduction settings is debated, and there is a lack of detailed studies on Li and B partitioning between minerals of different types of eclogites and the host rocks of the eclogites. We present Li and B concentration data of minerals and Li and B whole-rock isotope data for low-T and high-T eclogites and their phengite schist host rocks from the Changning–Menglian suture zone, SW China. Omphacite controls the Li budget in both the low-T and high-T eclogites. Low-T eclogites have Li and δ7Li values (8.4–27.0 ppm, – 5.5 to + 3.2 ‰) similar to the phengite schists (8.7–27.0 ppm, – 3.8 to + 3.0 ‰), suggesting that Li was added to low-T eclogites from the phengite schists. In contrast, high-T eclogites have much lower δ7Li values (– 13.2 to – 5.8 ‰) than the phengite schists, reflecting prograde loss of Li or exchange with wall rocks characterized by low δ7Li values. Phengite and retrograde amphibole/muscovite are the major B hosts for low-T and high-T eclogites, respectively. The budgets and isotopic compositions of B in eclogites are affected by the infiltration of fluids derived from phengite schists, as indicated by eclogite δ11B values (– 15.1 to – 8.1 ‰) overlapping with the values of the phengite schists (– 22.8 to – 9.5 ‰). Lithium and B in eclogites are hosted in different mineral phases that may have formed at different stages of metamorphism, implying that the contents and isotopic compositions of Li and B may become decoupled during subduction-related fluid-mediated redistribution. We suggest a mineralogical control on the redistribution of Li and B in eclogites during subduction and the exchange of Li and B with the immediate wall rocks. The observed contrasting Li and B isotopic signatures in eclogites are likely caused by a fluid-mediated exchange with different types of wall rocks during both prograde metamorphism and exhumation.

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The authors declare that the data supporting the findings of this study are available within the paper, and its supplementary information files.

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Acknowledgements

We gratefully acknowledge the assistance of Bettina Hübner (GFZ Potsdam) during the Li–B isotopic measurements, and also the work of Huawei Li (CAGS) and Zhiyong Zhu (CAGS) during the mineral trace element analyses by LA-ICPMS. Huining Wang and Jianjiang Zhu from CAGS are thanked for their help in preparing the samples. Discussions with Jia Cai and Jianbin Zheng (CAGS) are highly appreciated. We are grateful to Jianbin Zheng (CAGS) for sharing regional tectonic maps. We thank Paul Tomascak for truly helpful suggestions. We appreciate Enrico Cannaò and an anonymous reviewer for their constructive comments and Editor Daniela Rubatto for her thoughtful suggestions.

Funding

This study was financially supported by the National Natural Science Foundation of China [grant numbers 91855206, 40725007 and 42072221] and the Basic Research Foundation of the CAGS [grant numbers J2001 and J2302].

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Correspondence to Dan Wang.

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Communicated by Daniela Rubatto.

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Wang, D., Romer, R.L., Liu, F. et al. The behavior of Li and B isotopes in high-T and low-T eclogites enclosed by phengite schists. Contrib Mineral Petrol 179, 43 (2024). https://doi.org/10.1007/s00410-024-02124-1

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  • DOI: https://doi.org/10.1007/s00410-024-02124-1

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