High temperature fluid-rock interaction in oceanic crust: a study of fluid inclusions from the Trooso ophiolite and ODP/IODP Hole 1256D
Fluid inclusions offer the only available samples of uncontaminated sub-seafloor fluids. To date, microthermometry of such fluid inclusions trapped in ocean crust rocks has revealed that fluids of a wide range of salinities exist in both modem and ancient hydrothermal systems. LAICPMS analyses of fl...
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University of Leeds
2008
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.493781 |