Characterising low temperature alteration and oxidation of the upper oceanic crust
The circulation of low temperature hydrothermal fluids through the oceanic crust has signi�cant effects on the geochemical composition of the oceans and crust. Quantification of the magnitude and extent of these changes is essential for determining the crustal inputs to the mantle at subduction zone...
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University of Southampton
2015
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.640780 |