Woods Hole Oceanographic Institution

Maurice A Tivey

»Hydrothermal circulation within the Endeavour Segment; Juan de Fuca Ridge, G-cubed, 2010.
»Deep sea mining of seafloor massive sulfides, Marine Policy, 34, 2010.
»The Magnetic Signature of Hydrothermal Systems in Slow Spreading Environments
»A reduced crustal magnetization zone near the first observed active hydrothermal vent field on the Southwest Indian Ridge, Geophys. Res. Lett., 2010
»Origin of the Pacific Jurassic quiet zone,Geology, v. 34, 789-792, 2006
»Deep-tow magnetic anomaly study of the Pacific Jurassic Quiet Zone, JGR, 113, B07110, 2008.
»Central Anomaly Magnetization High East Pacific Rise (9 50' - 9 25'N), G-cubed, 2008.

Johnson, H.P., M.A. Tivey, T.A. Bjorkland and M.S. Salmi, Hydrothermal circulation within the Endeavour Segment; Juan de Fuca Ridge, Geochem. Geophys. Geosyst., 11(5), Q05002, doi:10.1029/2009GC002957, 2010

Areas of the seafloor at mid‐ocean ridges where hydrothermal vents discharge are easily recognized by the dramatic biological, physical, and chemical processes that characterize such sites. Locations where seawater flows into the seafloor to recharge hydrothermal cells within the crustal reservoir are by contrast almost invisible but can be indirectly identified by a systematic grid of conductive heat flow measurements.  An array of conductive heat flow stations in the Endeavour axial valley of the Juan de Fuca Ridge has identified recharge zones that appear to represent a nested system of fluid circulation paths.  At the scale of an axial rift valley, conductive heat flow data indicate a general cross‐valley fluid flow, where seawater enters the shallow subsurface crustal reservoir at the eastern wall of the Endeavour axial valley and undergoes a kilometer of horizontal transit beneath the valley floor, finally exiting as warm hydrothermal fluid discharge on the western valley bounding wall. Recharge zones also have been identified as located within an annular ring of very cold seafloor around the large Main Endeavour Hydrothermal Field, with seawater inflow occurring within faults that surround the fluid discharge sites. These conductive heat flow data are consistent with previous models where high‐temperature fluid circulation cells beneath large hydrothermal vent fields may be composed of narrow vertical cylinders. Subsurface fluid circulation on the Endeavour Segment occurs at various crustal depths in three distinct modes: (1) general east to west flow across the entire valley floor, (2) in narrow cylinders that penetrate deeply to high‐temperature heat sources, and (3) supplying low‐temperature diffuse vents where seawater is entrained into the shallow uppermost crust by the adjacent high‐temperature cylindrical systems. The systematic array of conductive heat flow measurements over the axial valley floor averaged ∼150 mW/m2, suggesting that only about 3% of the total energy flux of ocean crustal formation is removed by conductive heat transfer, with the remainder being dissipated to overlying seawater by fluid advection.

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