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Abstract. Massive sulfide samples have been recovered from Brothers and Rumble II West volcanoes of the southern Kermadec frontal arc, northeast of New Zealand. Both are caldera-forming volcanoes with Brothers largely dacitic and Rumble II West basaltic to basaltic-andesite in composition. The sulfide samples are considered to be pieces of chimneys from near the base of the caldera walls and are dominated...
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