Exploring the fate of Fe(III) at hydrothermal conditions
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Iron is the most abundant redox-active element in many rocks and geofluids. Yet, the redox chemistry of Fe in high temperature geofluids remains controversial. Comprehensive...
铁是诸多岩石与地热流体(geofluids)中丰度最高的氧化还原活性元素。然而,高温地热流体中铁的氧化还原化学行为仍存在争议。全面的……



