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    In:  Supplement to: Langseth, Marcus G; Ludwig, William J (1983): A heat flow measurement on the Falkland Plateau. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 299-303, https://doi.org/10.2973/dsdp.proc.71.109.1983
    Publication Date: 2019-04-30
    Description: At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole temperature measurements were made at 52.5 and 113 meters below the seafloor. The results show a regular increase of temperature with depth of 0.074 °C m**-1. Conductivity measurements on core samples, made on board ship and at the Lamont-Doherty repository, gave a mean value of 0.842 W °C**-1 m**-1. The heat flow indicated by these observations is 62.3 mW m**-2 (1.49 HFU), a value that is compatible with the geological evolution of the plateau.
    Type: Dataset
    Format: text/tab-separated-values, 93 data points
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