Abstract
At Hole 511, on the margin of Maurice Ewing Bank, successful bottom hole temperature measurements were made at 52.5 and 113m below the seafloor. The results show a regular increase of temperature with depth of 0.074oCm-1. Conductivity measurements on core samples, gave a mean value of 0.842W oC-1m-1. The heat flow indicated by these observations is 62.3mWm-2 (1.49HFU), a value that is compatible with the geological evolution of the plateau.-from Authors Hole 511 Maurice Ewing Bank bottom hole temperature measurements conductivity measurements on core samples geological evolution of the plate DSDP/ Leg71 Falkland Plateau
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CITATION STYLE
Langseth, M. G., & Ludwig, W. J. (1983). A heat flow measurement on the Falkland Plateau. Initial Reports DSDP, Leg 71, Valparaiso to Santos, 1980, Part 1, 299–303. https://doi.org/10.2973/dsdp.proc.71.109.1983
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