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Quaternary volcanic rocks from the New Britain island arc display a wide range in chemical compositions. The source of the lavas shares isotopic characteristics with Indian Ocean type mid-ocean ridge basalt (MORB). In contrast, the high field strength elements (HFSE) are extremely depleted in the volcanic front rocks compared with MORB. We propose that this results from a previous melt-extraction ...

Magma Genesis in the New Britain Island Arc: Further Insights into Melting and Mass Transfer Processes