俯冲带玻安岩研究进展

林若澜; 吴涛; 田丽艳; 鲁江姑

doi:10.3799/dqkx.2025.039

Volume 50 Issue 8

Aug. 2025

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Article Navigation > Earth Science > 2025 > 50(8): 2956-2976

Lin Ruolan, Wu Tao, Tian Liyan, Lu Jianggu, 2025. Progress in Subduction-Related Boninite Research. Earth Science, 50(8): 2956-2976. doi: 10.3799/dqkx.2025.039

Citation:

Lin Ruolan, Wu Tao, Tian Liyan, Lu Jianggu, 2025. Progress in Subduction-Related Boninite Research. Earth Science, 50(8): 2956-2976. doi: 10.3799/dqkx.2025.039

Lin Ruolan, Wu Tao, Tian Liyan, Lu Jianggu, 2025. Progress in Subduction-Related Boninite Research. Earth Science, 50(8): 2956-2976. doi: 10.3799/dqkx.2025.039

Citation:

Lin Ruolan, Wu Tao, Tian Liyan, Lu Jianggu, 2025. Progress in Subduction-Related Boninite Research. Earth Science, 50(8): 2956-2976. doi: 10.3799/dqkx.2025.039

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Progress in Subduction-Related Boninite Research

doi: 10.3799/dqkx.2025.039

Lin Ruolan^{1
,
,},
Wu Tao^{1, 2
,
,
,},
Tian Liyan³,
Lu Jianggu⁴

1.
Ocean College, Zhejiang University, Zhoushan 316022, China
2.
Hainan Institute of Zhejiang University, Sanya 572025, China
3.
Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China
4.
Key Laboratory of Submarine Geosciences, Ministry of Natural Resources, Hangzhou 310012, China

Received Date: 2025-02-01
Publish Date: 2025-08-25

Abstract

Abstract

Boninite is a special type of magnesium-iron volcanic rock, primarily formed in unique geological environments associated with plate subduction. It serves as a direct geological record of the subduction initiation. The phenocryst are mainly olivine and pyroxene, with no plagioclase. Boninite is characterized by high Mg and Si, but lower Ti content. They are also and enriched in large ion lithophile elements (LILEs) and light rare earth elements (LREEs), but depleted in high field strength elements (HFSEs) and medium rare earth elements (MREEs). Typicalboninite exhibits a distinctive "U"-shaped rare earth element (REE) distribution pattern.The unique chemical composition of boninite reflects its uniquemantle melting conditions, such as high temperature, low pressure, and relatively high water content.Primarymagma was generated throughre-melting processes in the mantle source, which has already undergone partial melting before. This unique melting process provides crucial insights into mantle source composition, degree of melting, and the role of fluids in mantle melting and the initiation of subduction.In this review, we discuss the mineralogy, geochemical characteristics, and petrogenetic mechanisms of subduction-related boninite, emphasizing its significance in geodynamics and magma evolution processes. Finally, we also summarized the current research issuesand potential future directions in boninite studies.
- boninite,
- geochemistry,
- petrogenesis,
- mantle melting,
- subduction initiation,
- subduction zone

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References(115)

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