Abstract: Hydrothermal circulation along oceanic detachment fault: Constraints on the nature and conditions of syntectonic silicification at the 13°20’N oceanic core complex (Mid-Atlantic ridge) (2016 AGU Fall Meeting)

Hydrothermal circulation along oceanic detachment fault: Constraints on the nature and conditions of syntectonic silicification at the 13°20’N oceanic core complex (Mid-Atlantic ridge)

Diane Bonnemains¹, Anne Verlaguet², Javier Escartin³, Catherine Mevel¹ and Muriel Andreani⁴, (1)Institut de Physique du Globe de Paris, Paris, France, (2)Organization Not Listed, Washington, DC, United States, (3)Institut de Physique du Globe, Paris, France, (4)University Claude Bernard Lyon 1, Villeurbanne, France

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