A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions.
Li X, Ishizuka O, Stern RJ, Li S, Lai Z, Somerville I, Suo Y, Chen L, Yu H.
Li X, et al.
Nat Commun. 2024 May 14;15(1):4088. doi: 10.1038/s41467-024-48308-y.
Nat Commun. 2024.
PMID: 38744830
Free PMC article.
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 …
However, the contribution of subducted components to the mantle source during initial arc rifting before back-arc basin spreading is not yet …