Fluid transport and reaction processes within a serpentinite mud volcano: South Chamorro Seamount

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Borehole observations of fluid flow from South Chamorro Seamount, an active serpentinite mud volcano in the Mariana forearc

A sealed borehole observatory (CORK) was deployed on South Chamorro Seamount, an active serpentinite mud volcano in the Mariana forearc to explore subduction-related processes on a non-accretionary, convergent plate margin. Formation fluid was overpressured relative to ambient hydrostatic conditions. Fluid flowed from the borehole at ~0.2 L/s when the observatory was opened to recover instrumen...

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ژورنال

عنوان ژورنال: Geochimica et Cosmochimica Acta

سال: 2020

ISSN: 0016-7037

DOI: 10.1016/j.gca.2019.10.037