An &lsquo;extinct&rsquo; transform fault hosts fluid flow and methane seepage &ndash; implications for understanding the role of transform faults in mid-ocean ridge fluid cycling

Kate Waghorn; Claudio Argentino; Sunil Vadakkepuliyambatta; Stefan Bünz; Giuliana Panieri; Andreia Plaza-Faverola

doi:https://doi.org/10.5194/egusphere-egu22-12108

[Back] [Session GMPV6.3]

EGU22-12108

https://doi.org/10.5194/egusphere-egu22-12108

EGU General Assembly 2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

An ‘extinct’ transform fault hosts fluid flow and methane seepage – implications for understanding the role of transform faults in mid-ocean ridge fluid cycling

Kate Waghorn¹, Claudio Argentino¹, Sunil Vadakkepuliyambatta², Stefan Bünz¹, Giuliana Panieri¹, and Andreia Plaza-Faverola¹

Kate Waghorn et al.

¹CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, 9037 Tromsø, Norway
²National Centre for Polar and Ocean Research (NCPOR), Ministry of Earth Sciences, Vasco-da-Gama, Goa, India

How to cite: Waghorn, K., Argentino, C., Vadakkepuliyambatta, S., Bünz, S., Panieri, G., and Plaza-Faverola, A.: An ‘extinct’ transform fault hosts fluid flow and methane seepage – implications for understanding the role of transform faults in mid-ocean ridge fluid cycling , EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-12108, https://doi.org/10.5194/egusphere-egu22-12108, 2022.

This abstract has been withdrawn on 11 May 2022.