Mineral reactions and isotopic tracer transport in the Troodos ophiolite as analogues of hydrothermal systems at mid-ocean ridges
The structure and evolution of mid-ocean ridge hydrothermal systems and the magnitude of crustal alteration associated with different temperature fluid fluxes are poorly understood. This project has used strontium and oxygen isotopes together with metamorphic assemblages to investigate fluid flow ge...
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University of Cambridge
1997
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.596622 |