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Two brine-charged sites (GB425 and GC233) at the northern Gulf of Mexico (GOM) continental slope were studied for their pore-water advective flow rates and stable carbon isotope geochemistry. Using chloride as a conservative tracer, a pore-water diffusion–advection model suggests that advection dominates pore-water flow in the upper 17cm sediments at both sites. Moreover, modeled results indicate...
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