An unequivocal case for high Nusselt number hydrothermal convection in sediment-buried igneous oceanic crust

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Keywords: heat flow; hydrothermal conditions; oceanic crust; permeability

Document Type: Research Article

DOI: http://dx.doi.org/10.1016/S0012-821X(96)00212-9

Affiliations: Pacific Geoscience Centre, Geological Survey of Canada, Box 6000, Sidney, B.C. V8L 4B2, Canada

Publication date: January 1, 1997

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