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A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions

Author

Listed:
  • Xiaohui Li

    (Ocean University of China
    Qingdao Marine Science and Technology Center
    Chinese Academy of Sciences)

  • Osamu Ishizuka

    (Geological Survey of Japan/AIST
    Japan Agency for Marine-Earth Science and Technology)

  • Robert J. Stern

    (University of Texas at Dallas)

  • Sanzhong Li

    (Ocean University of China
    Qingdao Marine Science and Technology Center)

  • Zhiqing Lai

    (Ocean University of China)

  • Ian Somerville

    (University College Dublin, Belfield)

  • Yanhui Suo

    (Ocean University of China
    Qingdao Marine Science and Technology Center)

  • Long Chen

    (Ocean University of China
    Qingdao Marine Science and Technology Center)

  • Hongxia Yu

    (Guilin University of Technology)

Abstract

Compositions of island arc and back-arc basin basalts are often used to trace the recycling of subducted materials. However, the contribution of subducted components to the mantle source during initial arc rifting before back-arc basin spreading is not yet well constrained. The northernmost Mariana arc is ideal for studying this because the transition from rifting to back-arc spreading is happening here. Here we report major and trace element and Pb isotopic compositions of olivine-hosted melt inclusions from lavas erupted during initial rifting at 24°N (NSP-24) and compare them with those in active arc front at 21°N and mature back-arc basin at 18°N. NSP-24 high-K melt inclusions have highly radiogenic Pb compositions and are close to those of the HIMU end-member, suggesting the presence of this component in the magma source. The HIMU-like component may be stored in the over-riding plate and released into arc magma with rifting. HIMU-type seamounts may be subducted elsewhere beneath the Mariana arc, but obvious HIMU-type components appear only in the initial stages of arc rifting due to the low melting degree and being consumed during the process of back-arc spreading.

Suggested Citation

  • Xiaohui Li & Osamu Ishizuka & Robert J. Stern & Sanzhong Li & Zhiqing Lai & Ian Somerville & Yanhui Suo & Long Chen & Hongxia Yu, 2024. "A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions," Nature Communications, Nature, vol. 15(1), pages 1-11, December.
    • Handle: RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-48308-y
    DOI: 10.1038/s41467-024-48308-y
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    References listed on IDEAS

    as
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