Anomalous heat flow in the northwest Atlantic: A case for continued hydrothermal circulation in 80-M.Y. crust
A detailed study of a 60×150 km area at 60°W, 24°N at the eastern end of the Nares Abyssal Plain indicates that hydrothermal circulation is still active in the 80 m.y. B.P. oceanic crust. The 58 heat flow measurements made at five stations in the area have revealed (1) constant heat flow over the ab...
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Columbia University
1983
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Online Access: | https://dx.doi.org/10.7916/d8pr7vrp https://academiccommons.columbia.edu/doi/10.7916/D8PR7VRP |