Evidence of degassing-induced oxidation of relatively oxidized K-rich magmas caused by degassing of dissolved SO<SUB>4</SUB><SUP>2-</SUP> (S<SUP>6+</SUP>) component in the melt to SO<SUB>2</SUB> (S<SUP>4+</SUP>) in the gas phase
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W[2016AGUFM.V31C3109P]
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