Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15d20'N fracture zone and the Mid-Atlantic Ridge

Details Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15d20'N fracture zone and the Mid-Atlantic Ridge Intense CH4 plumes generated by serpentinization of ultramafic rocks at the intersection of the 15d20'N fracture zone and the Mid-Atlantic Ridge

Jul 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998gecoa..62.2323c&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 62, p. 2323-2333.

Physics

27

Scientific paper

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