4.7 Article

Origin of the Mussau Trench in the Western Pacific: Geochemical and mineralogical constraints from basalts and serpentinized peridotites

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Summary: This study investigates the mineralogy and geochemistry of serpentinized peridotites from the Yap-Mariana Junction, and finds two distinct groups of samples. One group displays characteristics similar to abyssal peridotites, while the other group is more similar to forearc peridotites. This suggests a tectonic transition from a back-arc spreading ridge to a subduction zone in this region.

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