Low-temperature hydrothermal fluid flow using geochemical tracers, Juan de Fuca Ridge flank, N.E. Pacific Ocean
Fluid flow through mid-ocean ridge <i>axes</i> has long been recognised by geophysical and geochemical methods as well as direct observations. However, hydrothermal circulation through mid-ocean ridge <i>flanks</i> is more difficult to study and quantify due to the lower temp...
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University of Cambridge
2002
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.604812 |