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Major and minor chemistry, Sr, Nd and Pb isotope ratios, water content and hydrogen isotope ratios of the backarc basin volcanic rocks taken from the active spreading ridge and surrounding area between 12°40′N and 13°15′N in the southern part of the Mariana Trough indicate a complex regional interplay of suprasubduction-zone magmatic sources.

Geochemical Characteristics of Active Backarc Basin Volcanism at the Southern End of the Mariana Trough