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Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15°20′N fracture zone and the Mid-Atlantic Ridge

Marine GeologyFracture ZoneEarth ScienceVolcanologyEngineeringIntense Ch4 PlumesContinental TectonicsSubduction ZoneGeologyGeochemistryUltramafic RocksPetrologyTectonics