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Different TDM/CH 4 hydrothermal plume signatures: TAG site at 26°N and serpentinized ultrabasic diapir at 15°05'N on the Mid-Atlantic Ridge
FAMOUS and AMAR segments on the Mid-Atlantic Ridge: ubiquitous hydrothermal Mn, CH 4 , 3 He signals along the rift valley walls and rift offsets
Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15d20'N fracture zone and the Mid-Atlantic Ridge
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