The reactivity and isotopic fractionation of Fe-bearing minerals during sulfidation : an experimental approach
The presence of Fe bearing minerals at the sediment-water interface (within marine settings) promotes a variety of biological and abiological redox reactions during early diagenesis. The highly reactive nature of a portion of these Fe bearing minerals, with respect to organic and inorganic species,...
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University of Newcastle Upon Tyne
2011
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Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.566857 |