Quest for Fluid Flow along the Gloria Fault – First results of R/V Meteor expedition 162
- 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany (chensen@geomar.de)
- 2IPMA Portuguese Institute for Sea and Atmosphere, Lisbon, Portugal
- 3IDL Instituto Dom Luiz, Faculty of Science, University of Lisbon, Lisbon, Portugal
- 4Faculty of Geosciences, Bremen University, Bremen, Germany
- 5EAWAG Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland
- 6Institute of Geophysics, University of Hamburg, Hamburg, Germany
- 7Department of Environmental Systems Science, ETH Zürich, Zürich, Switzerland
Vast areas of the deep ocean floor are still insufficiently explored with respect to tectonic processes, exchange processes between the lithosphere and the ocean, and potential deep chemosynthetic energy sources for life. Transform faults and fracture zones, which are dominant seafloor morphological features in the abyssal ocean, deserve specific attention in this regard as they provide potential pathways for fluid recycling. One of them is the Gloria Fault, a unique feature in the Central North Atlantic. It has been the source of large magnitude earthquakes (namely the 1941, M8.4, the second largest instrumental earthquake on a fracture zone) and is a special case of a plate boundary, corresponding to the transform reactivation of an old oceanic fracture zone. Seismic refraction has shown an anomalous layer between normal lower crust and uppermost mantle, possibly a 4 km thick layer of hydrated mantle. We present first results of RV Meteor cruise M162 (March-April 2020) dedicated to the groundtruthing of potential fluid emanation sites.
How to cite: Hensen, C., Terrinha, P., Duarte, J., Kaul, N., Schmidt, M., Schmidt, C., Batista, L., Magalhāes, V., Liebetrau, V., Kipfer, R., Hübscher, C., and Lever, M.: Quest for Fluid Flow along the Gloria Fault – First results of R/V Meteor expedition 162, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8034, https://doi.org/10.5194/egusphere-egu2020-8034, 2020.
This abstract will not be presented.