Estimating mud expulsion rates from temperature measurements on Hakon Mosby Mud Volcano, SW Barents Sea

• Published in: Marine Geology
• Main Authors: Kaul, Norbert, Foucher, Jean-paul, Heesemann, M
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2006
• Subjects: SW Barents Sea; Convection; Heat flow; Mud volcano; Seafloor hydrothermal system; Barents Sea; Inner Crater; Svalbard
• Online Access: https://archimer.ifremer.fr/doc/2006/publication-2002.pdf; https://doi.org/10.1016/j.margeo.2006.02.004; https://archimer.ifremer.fr/doc/00000/2002/

The HAkon Mosby Mud Volcano (HMMV), located on the Norwegian-Barents-Svalbard continental margin in 1250 m water depth, has been identified and described as a structure caused by upward transport of mud, pore water and gas [e.g. Eldhohn, O., Sundvor, E., Vogt, P.R., Hjelstuen, B.O., Crane, K., Nilse...