@misc{langseth1983ttca, author={Marcus G {Langseth} and William J {Ludwig}}, title={{(Table 1) Thermal conductivity and water content at DSDP Hole 71-511}}, year={1983}, doi={10.1594/PANGAEA.813396}, url={https://doi.org/10.1594/PANGAEA.813396}, note={Supplement to: Langseth, MG; Ludwig, WJ (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}, abstract={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 {\textdegree}C m$\ast$$\ast$-1.\\ Conductivity measurements on core samples, made on board ship and at the Lamont-Doherty repository, gave a mean value of 0.842 W {\textdegree}C$\ast$$\ast$-1 m$\ast$$\ast$-1. The heat flow indicated by these observations is 62.3 mW m$\ast$$\ast$-2 (1.49 HFU), a value that is compatible with the geological evolution of the plateau.}, type={data set}, publisher={PANGAEA} }