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This work was supported by a Natural Environment Research Council (NE/H012648/1) and a Natural Environment Research Council Ion Microprobe Facility award. S.S. acknowledges Trinity Hall (Cambridge, UK) for providing a Mann Studentship towards her PhD studies. The Centre for Physics of Geological Processes, University of Oslo, provided the fieldwork funding.

Magmas Erupted during the Main Pulse of Siberian Traps Volcanism were Volatile-poor